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Downward spectral solar radiance as measured in different depths under sea ice (transmitted radiance) at station ALERT2018_17_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_17_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Radiance, downward; Radiance, downward, photosynthetically active; Radiance, downward, photosynthetically active, absolute; Remote operated vehicle; ROV; Sampling on land; Spectral radiance, downward at 320 nm; Spectral radiance, downward at 321 nm; Spectral radiance, downward at 322 nm; Spectral radiance, downward at 323 nm; Spectral radiance, downward at 324 nm; Spectral radiance, downward at 325 nm; Spectral radiance, downward at 326 nm; Spectral radiance, downward at 327 nm; Spectral radiance, downward at 328 nm; Spectral radiance, downward at 329 nm; Spectral radiance, downward at 330 nm; Spectral radiance, downward at 331 nm; Spectral radiance, downward at 332 nm; Spectral radiance, downward at 333 nm; Spectral radiance, downward at 334 nm; Spectral radiance, downward at 335 nm; Spectral radiance, downward at 336 nm; Spectral radiance, downward at 337 nm; Spectral radiance, downward at 338 nm; Spectral radiance, downward at 339 nm; Spectral radiance, downward at 340 nm; Spectral radiance, downward at 341 nm; Spectral radiance, downward at 342 nm; Spectral radiance, downward at 343 nm; Spectral radiance, downward at 344 nm; Spectral radiance, downward at 345 nm; Spectral radiance, downward at 346 nm; Spectral radiance, downward at 347 nm; Spectral radiance, downward at 348 nm; Spectral radiance, downward at 349 nm; Spectral radiance, downward at 350 nm; Spectral radiance, downward at 351 nm; Spectral radiance, downward at 352 nm; Spectral radiance, downward at 353 nm; Spectral radiance, downward at 354 nm; Spectral radiance, downward at 355 nm; Spectral radiance, downward at 356 nm; Spectral radiance, downward at 357 nm; Spectral radiance, downward at 358 nm; Spectral radiance, downward at 359 nm; Spectral radiance, downward at 360 nm; Spectral radiance, downward at 361 nm; Spectral radiance, downward at 362 nm; Spectral radiance, downward at 363 nm; Spectral radiance, downward at 364 nm; Spectral radiance, downward at 365 nm; Spectral radiance, downward at 366 nm; Spectral radiance, downward at 367 nm; Spectral radiance, downward at 368 nm; Spectral radiance, downward at 369 nm; Spectral radiance, downward at 370 nm; Spectral radiance, downward at 371 nm; Spectral radiance, downward at 372 nm; Spectral radiance, downward at 373 nm; Spectral radiance, downward at 374 nm; Spectral radiance, downward at 375 nm; Spectral radiance, downward at 376 nm; Spectral radiance, downward at 377 nm; Spectral radiance, downward at 378 nm; Spectral radiance, downward at 379 nm; Spectral radiance, downward at 380 nm; Spectral radiance, downward at 381 nm; Spectral radiance, downward at 382 nm; Spectral radiance, downward at 383 nm; Spectral radiance, downward at 384 nm; Spectral radiance, downward at 385 nm; Spectral radiance, downward at 386 nm; Spectral radiance, downward at 387 nm; Spectral radiance, downward at 388 nm; Spectral radiance, downward at 389 nm; Spectral radiance, downward at 390 nm; Spectral radiance, downward at 391 nm; Spectral radiance, downward at 392 nm; Spectral radiance, downward at 393 nm; Spectral radiance, downward at 394 nm; Spectral radiance, downward at 395 nm; Spectral radiance, downward at 396 nm; Spectral radiance, downward at 397 nm; Spectral radiance, downward at 398 nm; Spectral radiance, downward at 399 nm; Spectral radiance, downward at 400 nm; Spectral radiance, downward at 401 nm; Spectral radiance, downward at 402 nm; Spectral radiance, downward at 403 nm; Spectral radiance, downward at 404 nm; Spectral radiance, downward at 405 nm; Spectral radiance, downward at 406 nm; Spectral radiance, downward at 407 nm; Spectral radiance, downward at 408 nm; Spectral radiance, downward at 409 nm; Spectral radiance, downward at 410 nm; Spectral radiance, downward at 411 nm; Spectral radiance, downward at 412 nm; Spectral radiance, downward at 413 nm; Spectral radiance, downward at 414 nm; Spectral radiance, downward at 415 nm; Spectral radiance, downward at 416 nm; Spectral radiance, downward at 417 nm; Spectral radiance, downward at 418 nm; Spectral radiance, downward at 419 nm; Spectral radiance, downward at 420 nm; Spectral radiance, downward at 421 nm; Spectral radiance, downward at 422 nm; Spectral radiance, downward at 423 nm; Spectral radiance, downward at 424 nm; Spectral radiance, downward at 425 nm; Spectral radiance, downward at 426 nm; Spectral radiance, downward at 427 nm; Spectral radiance, downward at 428 nm; Spectral radiance, downward at 429 nm; Spectral radiance, downward at 430 nm; Spectral radiance, downward at 431 nm; Spectral radiance, downward at 432 nm; Spectral radiance, downward at 433 nm; Spectral radiance, downward at 434 nm; Spectral radiance, downward at 435 nm; Spectral radiance, downward at 436 nm; Spectral radiance, downward at 437 nm; Spectral radiance, downward at 438 nm; Spectral radiance, downward at 439 nm; Spectral radiance, downward at 440 nm; Spectral radiance, downward at 441 nm; Spectral radiance, downward at 442 nm; Spectral radiance, downward at 443 nm; Spectral radiance, downward at 444 nm; Spectral radiance, downward at 445 nm; Spectral radiance, downward at 446 nm; Spectral radiance, downward at 447 nm; Spectral radiance, downward at 448 nm; Spectral radiance, downward at 449 nm; Spectral radiance, downward at 450 nm; Spectral radiance, downward at 451 nm; Spectral radiance, downward at 452 nm; Spectral radiance, downward at 453 nm; Spectral radiance, downward at 454 nm; Spectral radiance, downward at 455 nm; Spectral radiance, downward at 456 nm; Spectral radiance, downward at 457 nm; Spectral radiance, downward at 458 nm; Spectral radiance, downward at 459 nm; Spectral radiance, downward at 460 nm; Spectral radiance, downward at 461 nm; Spectral radiance, downward at 462 nm; Spectral radiance, downward at 463 nm; Spectral radiance, downward at 464 nm; Spectral radiance, downward at 465 nm; Spectral radiance, downward at 466 nm; Spectral radiance, downward at 467 nm; Spectral radiance, downward at 468 nm; Spectral radiance, downward at 469 nm; Spectral radiance, downward at 470 nm; Spectral radiance, downward at 471 nm; Spectral radiance, downward at 472 nm; Spectral radiance, downward at 473 nm; Spectral radiance, downward at 474 nm; Spectral radiance, downward at 475 nm; Spectral radiance, downward at 476 nm; Spectral radiance, downward at 477 nm; Spectral radiance, downward at 478 nm; Spectral radiance, downward at 479 nm; Spectral radiance, downward at 480 nm; Spectral radiance, downward at 481 nm; Spectral radiance, downward at 482 nm; Spectral radiance, downward at 483 nm; Spectral radiance, downward at 484 nm; Spectral radiance, downward at 485 nm; Spectral radiance, downward at 486 nm; Spectral radiance, downward at 487 nm; Spectral radiance, downward at 488 nm; Spectral radiance, downward at 489 nm; Spectral radiance, downward at 490 nm; Spectral radiance, downward at 491 nm; Spectral radiance, downward at 492 nm; Spectral radiance, downward at 493 nm; Spectral radiance, downward at 494 nm; Spectral radiance, downward at 495 nm; Spectral radiance, downward at 496 nm; Spectral radiance, downward at 497 nm; Spectral radiance, downward at 498 nm; Spectral radiance, downward at 499 nm; Spectral radiance, downward at 500 nm; Spectral radiance, downward at 501 nm; Spectral radiance, downward at 502 nm; Spectral radiance, downward at 503 nm; Spectral radiance, downward at 504 nm; Spectral radiance, downward at 505 nm; Spectral radiance, downward at 506 nm; Spectral radiance, downward at 507 nm; Spectral radiance, downward at 508 nm; Spectral radiance, downward at 509 nm; Spectral radiance, downward at 510 nm; Spectral radiance, downward at 511 nm; Spectral radiance, downward at 512 nm; Spectral radiance, downward at 513 nm; Spectral radiance, downward at 514 nm; Spectral radiance,

Type: Dataset

Format: text/tab-separated-values, 2778678 data points

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Positioning of ROV at station ALERT2018_08_2 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_08_2; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Heading; LATITUDE; Lincoln Sea; LONGITUDE; Pitch angle; Remote operated vehicle; Roll angle; ROV; Sampling on land

Type: Dataset

Format: text/tab-separated-values, 30965 data points

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103

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Downward spectral solar radiance as measured in different depths under sea ice (transmitted radiance) at station ALERT2018_19_2 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_19_2; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Radiance, downward; Radiance, downward, photosynthetically active; Radiance, downward, photosynthetically active, absolute; Remote operated vehicle; ROV; Sampling on land; Spectral radiance, downward at 320 nm; Spectral radiance, downward at 321 nm; Spectral radiance, downward at 322 nm; Spectral radiance, downward at 323 nm; Spectral radiance, downward at 324 nm; Spectral radiance, downward at 325 nm; Spectral radiance, downward at 326 nm; Spectral radiance, downward at 327 nm; Spectral radiance, downward at 328 nm; Spectral radiance, downward at 329 nm; Spectral radiance, downward at 330 nm; Spectral radiance, downward at 331 nm; Spectral radiance, downward at 332 nm; Spectral radiance, downward at 333 nm; Spectral radiance, downward at 334 nm; Spectral radiance, downward at 335 nm; Spectral radiance, downward at 336 nm; Spectral radiance, downward at 337 nm; Spectral radiance, downward at 338 nm; Spectral radiance, downward at 339 nm; Spectral radiance, downward at 340 nm; Spectral radiance, downward at 341 nm; Spectral radiance, downward at 342 nm; Spectral radiance, downward at 343 nm; Spectral radiance, downward at 344 nm; Spectral radiance, downward at 345 nm; Spectral radiance, downward at 346 nm; Spectral radiance, downward at 347 nm; Spectral radiance, downward at 348 nm; Spectral radiance, downward at 349 nm; Spectral radiance, downward at 350 nm; Spectral radiance, downward at 351 nm; Spectral radiance, downward at 352 nm; Spectral radiance, downward at 353 nm; Spectral radiance, downward at 354 nm; Spectral radiance, downward at 355 nm; Spectral radiance, downward at 356 nm; Spectral radiance, downward at 357 nm; Spectral radiance, downward at 358 nm; Spectral radiance, downward at 359 nm; Spectral radiance, downward at 360 nm; Spectral radiance, downward at 361 nm; Spectral radiance, downward at 362 nm; Spectral radiance, downward at 363 nm; Spectral radiance, downward at 364 nm; Spectral radiance, downward at 365 nm; Spectral radiance, downward at 366 nm; Spectral radiance, downward at 367 nm; Spectral radiance, downward at 368 nm; Spectral radiance, downward at 369 nm; Spectral radiance, downward at 370 nm; Spectral radiance, downward at 371 nm; Spectral radiance, downward at 372 nm; Spectral radiance, downward at 373 nm; Spectral radiance, downward at 374 nm; Spectral radiance, downward at 375 nm; Spectral radiance, downward at 376 nm; Spectral radiance, downward at 377 nm; Spectral radiance, downward at 378 nm; Spectral radiance, downward at 379 nm; Spectral radiance, downward at 380 nm; Spectral radiance, downward at 381 nm; Spectral radiance, downward at 382 nm; Spectral radiance, downward at 383 nm; Spectral radiance, downward at 384 nm; Spectral radiance, downward at 385 nm; Spectral radiance, downward at 386 nm; Spectral radiance, downward at 387 nm; Spectral radiance, downward at 388 nm; Spectral radiance, downward at 389 nm; Spectral radiance, downward at 390 nm; Spectral radiance, downward at 391 nm; Spectral radiance, downward at 392 nm; Spectral radiance, downward at 393 nm; Spectral radiance, downward at 394 nm; Spectral radiance, downward at 395 nm; Spectral radiance, downward at 396 nm; Spectral radiance, downward at 397 nm; Spectral radiance, downward at 398 nm; Spectral radiance, downward at 399 nm; Spectral radiance, downward at 400 nm; Spectral radiance, downward at 401 nm; Spectral radiance, downward at 402 nm; Spectral radiance, downward at 403 nm; Spectral radiance, downward at 404 nm; Spectral radiance, downward at 405 nm; Spectral radiance, downward at 406 nm; Spectral radiance, downward at 407 nm; Spectral radiance, downward at 408 nm; Spectral radiance, downward at 409 nm; Spectral radiance, downward at 410 nm; Spectral radiance, downward at 411 nm; Spectral radiance, downward at 412 nm; Spectral radiance, downward at 413 nm; Spectral radiance, downward at 414 nm; Spectral radiance, downward at 415 nm; Spectral radiance, downward at 416 nm; Spectral radiance, downward at 417 nm; Spectral radiance, downward at 418 nm; Spectral radiance, downward at 419 nm; Spectral radiance, downward at 420 nm; Spectral radiance, downward at 421 nm; Spectral radiance, downward at 422 nm; Spectral radiance, downward at 423 nm; Spectral radiance, downward at 424 nm; Spectral radiance, downward at 425 nm; Spectral radiance, downward at 426 nm; Spectral radiance, downward at 427 nm; Spectral radiance, downward at 428 nm; Spectral radiance, downward at 429 nm; Spectral radiance, downward at 430 nm; Spectral radiance, downward at 431 nm; Spectral radiance, downward at 432 nm; Spectral radiance, downward at 433 nm; Spectral radiance, downward at 434 nm; Spectral radiance, downward at 435 nm; Spectral radiance, downward at 436 nm; Spectral radiance, downward at 437 nm; Spectral radiance, downward at 438 nm; Spectral radiance, downward at 439 nm; Spectral radiance, downward at 440 nm; Spectral radiance, downward at 441 nm; Spectral radiance, downward at 442 nm; Spectral radiance, downward at 443 nm; Spectral radiance, downward at 444 nm; Spectral radiance, downward at 445 nm; Spectral radiance, downward at 446 nm; Spectral radiance, downward at 447 nm; Spectral radiance, downward at 448 nm; Spectral radiance, downward at 449 nm; Spectral radiance, downward at 450 nm; Spectral radiance, downward at 451 nm; Spectral radiance, downward at 452 nm; Spectral radiance, downward at 453 nm; Spectral radiance, downward at 454 nm; Spectral radiance, downward at 455 nm; Spectral radiance, downward at 456 nm; Spectral radiance, downward at 457 nm; Spectral radiance, downward at 458 nm; Spectral radiance, downward at 459 nm; Spectral radiance, downward at 460 nm; Spectral radiance, downward at 461 nm; Spectral radiance, downward at 462 nm; Spectral radiance, downward at 463 nm; Spectral radiance, downward at 464 nm; Spectral radiance, downward at 465 nm; Spectral radiance, downward at 466 nm; Spectral radiance, downward at 467 nm; Spectral radiance, downward at 468 nm; Spectral radiance, downward at 469 nm; Spectral radiance, downward at 470 nm; Spectral radiance, downward at 471 nm; Spectral radiance, downward at 472 nm; Spectral radiance, downward at 473 nm; Spectral radiance, downward at 474 nm; Spectral radiance, downward at 475 nm; Spectral radiance, downward at 476 nm; Spectral radiance, downward at 477 nm; Spectral radiance, downward at 478 nm; Spectral radiance, downward at 479 nm; Spectral radiance, downward at 480 nm; Spectral radiance, downward at 481 nm; Spectral radiance, downward at 482 nm; Spectral radiance, downward at 483 nm; Spectral radiance, downward at 484 nm; Spectral radiance, downward at 485 nm; Spectral radiance, downward at 486 nm; Spectral radiance, downward at 487 nm; Spectral radiance, downward at 488 nm; Spectral radiance, downward at 489 nm; Spectral radiance, downward at 490 nm; Spectral radiance, downward at 491 nm; Spectral radiance, downward at 492 nm; Spectral radiance, downward at 493 nm; Spectral radiance, downward at 494 nm; Spectral radiance, downward at 495 nm; Spectral radiance, downward at 496 nm; Spectral radiance, downward at 497 nm; Spectral radiance, downward at 498 nm; Spectral radiance, downward at 499 nm; Spectral radiance, downward at 500 nm; Spectral radiance, downward at 501 nm; Spectral radiance, downward at 502 nm; Spectral radiance, downward at 503 nm; Spectral radiance, downward at 504 nm; Spectral radiance, downward at 505 nm; Spectral radiance, downward at 506 nm; Spectral radiance, downward at 507 nm; Spectral radiance, downward at 508 nm; Spectral radiance, downward at 509 nm; Spectral radiance, downward at 510 nm; Spectral radiance, downward at 511 nm; Spectral radiance, downward at 512 nm; Spectral radiance, downward at 513 nm; Spectral radiance, downward at 514 nm; Spectral radiance,

Type: Dataset

Format: text/tab-separated-values, 2538889 data points

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at station ALERT2018_08_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_08_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transmittance; Transmittance, photosynthetically active; Transmittance at 320 nm; Transmittance at 321 nm; Transmittance at 322 nm; Transmittance at 323 nm; Transmittance at 324 nm; Transmittance at 325 nm; Transmittance at 326 nm; Transmittance at 327 nm; Transmittance at 328 nm; Transmittance at 329 nm; Transmittance at 330 nm; Transmittance at 331 nm; Transmittance at 332 nm; Transmittance at 333 nm; Transmittance at 334 nm; Transmittance at 335 nm; Transmittance at 336 nm; Transmittance at 337 nm; Transmittance at 338 nm; Transmittance at 339 nm; Transmittance at 340 nm; Transmittance at 341 nm; Transmittance at 342 nm; Transmittance at 343 nm; Transmittance at 344 nm; Transmittance at 345 nm; Transmittance at 346 nm; Transmittance at 347 nm; Transmittance at 348 nm; Transmittance at 349 nm; Transmittance at 350 nm; Transmittance at 351 nm; Transmittance at 352 nm; Transmittance at 353 nm; Transmittance at 354 nm; Transmittance at 355 nm; Transmittance at 356 nm; Transmittance at 357 nm; Transmittance at 358 nm; Transmittance at 359 nm; Transmittance at 360 nm; Transmittance at 361 nm; Transmittance at 362 nm; Transmittance at 363 nm; Transmittance at 364 nm; Transmittance at 365 nm; Transmittance at 366 nm; Transmittance at 367 nm; Transmittance at 368 nm; Transmittance at 369 nm; Transmittance at 370 nm; Transmittance at 371 nm; Transmittance at 372 nm; Transmittance at 373 nm; Transmittance at 374 nm; Transmittance at 375 nm; Transmittance at 376 nm; Transmittance at 377 nm; Transmittance at 378 nm; Transmittance at 379 nm; Transmittance at 380 nm; Transmittance at 381 nm; Transmittance at 382 nm; Transmittance at 383 nm; Transmittance at 384 nm; Transmittance at 385 nm; Transmittance at 386 nm; Transmittance at 387 nm; Transmittance at 388 nm; Transmittance at 389 nm; Transmittance at 390 nm; Transmittance at 391 nm; Transmittance at 392 nm; Transmittance at 393 nm; Transmittance at 394 nm; Transmittance at 395 nm; Transmittance at 396 nm; Transmittance at 397 nm; Transmittance at 398 nm; Transmittance at 399 nm; Transmittance at 400 nm; Transmittance at 401 nm; Transmittance at 402 nm; Transmittance at 403 nm; Transmittance at 404 nm; Transmittance at 405 nm; Transmittance at 406 nm; Transmittance at 407 nm; Transmittance at 408 nm; Transmittance at 409 nm; Transmittance at 410 nm; Transmittance at 411 nm; Transmittance at 412 nm; Transmittance at 413 nm; Transmittance at 414 nm; Transmittance at 415 nm; Transmittance at 416 nm; Transmittance at 417 nm; Transmittance at 418 nm; Transmittance at 419 nm; Transmittance at 420 nm; Transmittance at 421 nm; Transmittance at 422 nm; Transmittance at 423 nm; Transmittance at 424 nm; Transmittance at 425 nm; Transmittance at 426 nm; Transmittance at 427 nm; Transmittance at 428 nm; Transmittance at 429 nm; Transmittance at 430 nm; Transmittance at 431 nm; Transmittance at 432 nm; Transmittance at 433 nm; Transmittance at 434 nm; Transmittance at 435 nm; Transmittance at 436 nm; Transmittance at 437 nm; Transmittance at 438 nm; Transmittance at 439 nm; Transmittance at 440 nm; Transmittance at 441 nm; Transmittance at 442 nm; Transmittance at 443 nm; Transmittance at 444 nm; Transmittance at 445 nm; Transmittance at 446 nm; Transmittance at 447 nm; Transmittance at 448 nm; Transmittance at 449 nm; Transmittance at 450 nm; Transmittance at 451 nm; Transmittance at 452 nm; Transmittance at 453 nm; Transmittance at 454 nm; Transmittance at 455 nm; Transmittance at 456 nm; Transmittance at 457 nm; Transmittance at 458 nm; Transmittance at 459 nm; Transmittance at 460 nm; Transmittance at 461 nm; Transmittance at 462 nm; Transmittance at 463 nm; Transmittance at 464 nm; Transmittance at 465 nm; Transmittance at 466 nm; Transmittance at 467 nm; Transmittance at 468 nm; Transmittance at 469 nm; Transmittance at 470 nm; Transmittance at 471 nm; Transmittance at 472 nm; Transmittance at 473 nm; Transmittance at 474 nm; Transmittance at 475 nm; Transmittance at 476 nm; Transmittance at 477 nm; Transmittance at 478 nm; Transmittance at 479 nm; Transmittance at 480 nm; Transmittance at 481 nm; Transmittance at 482 nm; Transmittance at 483 nm; Transmittance at 484 nm; Transmittance at 485 nm; Transmittance at 486 nm; Transmittance at 487 nm; Transmittance at 488 nm; Transmittance at 489 nm; Transmittance at 490 nm; Transmittance at 491 nm; Transmittance at 492 nm; Transmittance at 493 nm; Transmittance at 494 nm; Transmittance at 495 nm; Transmittance at 496 nm; Transmittance at 497 nm; Transmittance at 498 nm; Transmittance at 499 nm; Transmittance at 500 nm; Transmittance at 501 nm; Transmittance at 502 nm; Transmittance at 503 nm; Transmittance at 504 nm; Transmittance at 505 nm; Transmittance at 506 nm; Transmittance at 507 nm; Transmittance at 508 nm; Transmittance at 509 nm; Transmittance at 510 nm; Transmittance at 511 nm; Transmittance at 512 nm; Transmittance at 513 nm; Transmittance at 514 nm; Transmittance at 515 nm; Transmittance at 516 nm; Transmittance at 517 nm; Transmittance at 518 nm; Transmittance at 519 nm; Transmittance at 520 nm; Transmittance at 521 nm; Transmittance at 522 nm; Transmittance at 523 nm; Transmittance at 524 nm; Transmittance at 525 nm; Transmittance at 526 nm; Transmittance at 527 nm; Transmittance at 528 nm; Transmittance at 529 nm; Transmittance at 530 nm; Transmittance at 531 nm; Transmittance at 532 nm; Transmittance at 533 nm; Transmittance at 534 nm; Transmittance at 535 nm; Transmittance at 536 nm; Transmittance at 537 nm; Transmittance at 538 nm; Transmittance at 539 nm; Transmittance at 540 nm; Transmittance at 541 nm; Transmittance at 542 nm; Transmittance at 543 nm; Transmittance at 544 nm; Transmittance at 545 nm; Transmittance at 546 nm; Transmittance at 547 nm; Transmittance at 548 nm; Transmittance at 549 nm; Transmittance at 550 nm; Transmittance at 551 nm; Transmittance at 552 nm; Transmittance at 553 nm; Transmittance at 554 nm; Transmittance at 555 nm; Transmittance at 556 nm; Transmittance at 557 nm; Transmittance at 558 nm; Transmittance at 559 nm; Transmittance at 560 nm; Transmittance at 561 nm; Transmittance at 562 nm; Transmittance at 563 nm; Transmittance at 564 nm; Transmittance at 565 nm; Transmittance at 566 nm; Transmittance at 567 nm; Transmittance at 568 nm; Transmittance at 569 nm; Transmittance at 570 nm; Transmittance at 571 nm; Transmittance at 572 nm; Transmittance at 573 nm; Transmittance at 574 nm; Transmittance at 575 nm; Transmittance at 576 nm; Transmittance at 577 nm; Transmittance at 578 nm; Transmittance at 579 nm; Transmittance at 580 nm; Transmittance at 581 nm; Transmittance at 582 nm; Transmittance at 583 nm; Transmittance at 584 nm; Transmittance at 585 nm; Transmittance at 586 nm; Transmittance at 587 nm; Transmittance at 588 nm; Transmittance at 589 nm; Transmittance at 590 nm; Transmittance at 591 nm; Transmittance at 592 nm; Transmittance at 593 nm; Transmittance at 594 nm; Transmittance at 595 nm; Transmittance at 596 nm; Transmittance at 597 nm; Transmittance at 598 nm; Transmittance at 599 nm; Transmittance at 600 nm; Transmittance at 601 nm; Transmittance at 602 nm; Transmittance at 603 nm; Transmittance at 604 nm; Transmittance at 605 nm; Transmittance at 606 nm; Transmittance at 607 nm; Transmittance at 608 nm; Transmittance at 609 nm; Transmittance at 610 nm; Transmittance at 611 nm; Transmittance at 612 nm; Transmittance at 613 nm; Transmittance at 614 nm; Transmittance at 615 nm; Transmittance at 616 nm; Transmittance at 617 nm; Transmittance at 618 nm; Transmittance at 619 nm; Transmittance at 620 nm; Transmittance at 621 nm; Transmittance at 622 nm; Transmittance at 623 nm; Transmittance at 624 nm; Transmittance at 625 nm; Transmittance at 626 nm; Transmittance at

Type: Dataset

Format: text/tab-separated-values, 381635 data points

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at station ALERT2018_08_2 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_08_2; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transmittance; Transmittance, photosynthetically active; Transmittance at 320 nm; Transmittance at 321 nm; Transmittance at 322 nm; Transmittance at 323 nm; Transmittance at 324 nm; Transmittance at 325 nm; Transmittance at 326 nm; Transmittance at 327 nm; Transmittance at 328 nm; Transmittance at 329 nm; Transmittance at 330 nm; Transmittance at 331 nm; Transmittance at 332 nm; Transmittance at 333 nm; Transmittance at 334 nm; Transmittance at 335 nm; Transmittance at 336 nm; Transmittance at 337 nm; Transmittance at 338 nm; Transmittance at 339 nm; Transmittance at 340 nm; Transmittance at 341 nm; Transmittance at 342 nm; Transmittance at 343 nm; Transmittance at 344 nm; Transmittance at 345 nm; Transmittance at 346 nm; Transmittance at 347 nm; Transmittance at 348 nm; Transmittance at 349 nm; Transmittance at 350 nm; Transmittance at 351 nm; Transmittance at 352 nm; Transmittance at 353 nm; Transmittance at 354 nm; Transmittance at 355 nm; Transmittance at 356 nm; Transmittance at 357 nm; Transmittance at 358 nm; Transmittance at 359 nm; Transmittance at 360 nm; Transmittance at 361 nm; Transmittance at 362 nm; Transmittance at 363 nm; Transmittance at 364 nm; Transmittance at 365 nm; Transmittance at 366 nm; Transmittance at 367 nm; Transmittance at 368 nm; Transmittance at 369 nm; Transmittance at 370 nm; Transmittance at 371 nm; Transmittance at 372 nm; Transmittance at 373 nm; Transmittance at 374 nm; Transmittance at 375 nm; Transmittance at 376 nm; Transmittance at 377 nm; Transmittance at 378 nm; Transmittance at 379 nm; Transmittance at 380 nm; Transmittance at 381 nm; Transmittance at 382 nm; Transmittance at 383 nm; Transmittance at 384 nm; Transmittance at 385 nm; Transmittance at 386 nm; Transmittance at 387 nm; Transmittance at 388 nm; Transmittance at 389 nm; Transmittance at 390 nm; Transmittance at 391 nm; Transmittance at 392 nm; Transmittance at 393 nm; Transmittance at 394 nm; Transmittance at 395 nm; Transmittance at 396 nm; Transmittance at 397 nm; Transmittance at 398 nm; Transmittance at 399 nm; Transmittance at 400 nm; Transmittance at 401 nm; Transmittance at 402 nm; Transmittance at 403 nm; Transmittance at 404 nm; Transmittance at 405 nm; Transmittance at 406 nm; Transmittance at 407 nm; Transmittance at 408 nm; Transmittance at 409 nm; Transmittance at 410 nm; Transmittance at 411 nm; Transmittance at 412 nm; Transmittance at 413 nm; Transmittance at 414 nm; Transmittance at 415 nm; Transmittance at 416 nm; Transmittance at 417 nm; Transmittance at 418 nm; Transmittance at 419 nm; Transmittance at 420 nm; Transmittance at 421 nm; Transmittance at 422 nm; Transmittance at 423 nm; Transmittance at 424 nm; Transmittance at 425 nm; Transmittance at 426 nm; Transmittance at 427 nm; Transmittance at 428 nm; Transmittance at 429 nm; Transmittance at 430 nm; Transmittance at 431 nm; Transmittance at 432 nm; Transmittance at 433 nm; Transmittance at 434 nm; Transmittance at 435 nm; Transmittance at 436 nm; Transmittance at 437 nm; Transmittance at 438 nm; Transmittance at 439 nm; Transmittance at 440 nm; Transmittance at 441 nm; Transmittance at 442 nm; Transmittance at 443 nm; Transmittance at 444 nm; Transmittance at 445 nm; Transmittance at 446 nm; Transmittance at 447 nm; Transmittance at 448 nm; Transmittance at 449 nm; Transmittance at 450 nm; Transmittance at 451 nm; Transmittance at 452 nm; Transmittance at 453 nm; Transmittance at 454 nm; Transmittance at 455 nm; Transmittance at 456 nm; Transmittance at 457 nm; Transmittance at 458 nm; Transmittance at 459 nm; Transmittance at 460 nm; Transmittance at 461 nm; Transmittance at 462 nm; Transmittance at 463 nm; Transmittance at 464 nm; Transmittance at 465 nm; Transmittance at 466 nm; Transmittance at 467 nm; Transmittance at 468 nm; Transmittance at 469 nm; Transmittance at 470 nm; Transmittance at 471 nm; Transmittance at 472 nm; Transmittance at 473 nm; Transmittance at 474 nm; Transmittance at 475 nm; Transmittance at 476 nm; Transmittance at 477 nm; Transmittance at 478 nm; Transmittance at 479 nm; Transmittance at 480 nm; Transmittance at 481 nm; Transmittance at 482 nm; Transmittance at 483 nm; Transmittance at 484 nm; Transmittance at 485 nm; Transmittance at 486 nm; Transmittance at 487 nm; Transmittance at 488 nm; Transmittance at 489 nm; Transmittance at 490 nm; Transmittance at 491 nm; Transmittance at 492 nm; Transmittance at 493 nm; Transmittance at 494 nm; Transmittance at 495 nm; Transmittance at 496 nm; Transmittance at 497 nm; Transmittance at 498 nm; Transmittance at 499 nm; Transmittance at 500 nm; Transmittance at 501 nm; Transmittance at 502 nm; Transmittance at 503 nm; Transmittance at 504 nm; Transmittance at 505 nm; Transmittance at 506 nm; Transmittance at 507 nm; Transmittance at 508 nm; Transmittance at 509 nm; Transmittance at 510 nm; Transmittance at 511 nm; Transmittance at 512 nm; Transmittance at 513 nm; Transmittance at 514 nm; Transmittance at 515 nm; Transmittance at 516 nm; Transmittance at 517 nm; Transmittance at 518 nm; Transmittance at 519 nm; Transmittance at 520 nm; Transmittance at 521 nm; Transmittance at 522 nm; Transmittance at 523 nm; Transmittance at 524 nm; Transmittance at 525 nm; Transmittance at 526 nm; Transmittance at 527 nm; Transmittance at 528 nm; Transmittance at 529 nm; Transmittance at 530 nm; Transmittance at 531 nm; Transmittance at 532 nm; Transmittance at 533 nm; Transmittance at 534 nm; Transmittance at 535 nm; Transmittance at 536 nm; Transmittance at 537 nm; Transmittance at 538 nm; Transmittance at 539 nm; Transmittance at 540 nm; Transmittance at 541 nm; Transmittance at 542 nm; Transmittance at 543 nm; Transmittance at 544 nm; Transmittance at 545 nm; Transmittance at 546 nm; Transmittance at 547 nm; Transmittance at 548 nm; Transmittance at 549 nm; Transmittance at 550 nm; Transmittance at 551 nm; Transmittance at 552 nm; Transmittance at 553 nm; Transmittance at 554 nm; Transmittance at 555 nm; Transmittance at 556 nm; Transmittance at 557 nm; Transmittance at 558 nm; Transmittance at 559 nm; Transmittance at 560 nm; Transmittance at 561 nm; Transmittance at 562 nm; Transmittance at 563 nm; Transmittance at 564 nm; Transmittance at 565 nm; Transmittance at 566 nm; Transmittance at 567 nm; Transmittance at 568 nm; Transmittance at 569 nm; Transmittance at 570 nm; Transmittance at 571 nm; Transmittance at 572 nm; Transmittance at 573 nm; Transmittance at 574 nm; Transmittance at 575 nm; Transmittance at 576 nm; Transmittance at 577 nm; Transmittance at 578 nm; Transmittance at 579 nm; Transmittance at 580 nm; Transmittance at 581 nm; Transmittance at 582 nm; Transmittance at 583 nm; Transmittance at 584 nm; Transmittance at 585 nm; Transmittance at 586 nm; Transmittance at 587 nm; Transmittance at 588 nm; Transmittance at 589 nm; Transmittance at 590 nm; Transmittance at 591 nm; Transmittance at 592 nm; Transmittance at 593 nm; Transmittance at 594 nm; Transmittance at 595 nm; Transmittance at 596 nm; Transmittance at 597 nm; Transmittance at 598 nm; Transmittance at 599 nm; Transmittance at 600 nm; Transmittance at 601 nm; Transmittance at 602 nm; Transmittance at 603 nm; Transmittance at 604 nm; Transmittance at 605 nm; Transmittance at 606 nm; Transmittance at 607 nm; Transmittance at 608 nm; Transmittance at 609 nm; Transmittance at 610 nm; Transmittance at 611 nm; Transmittance at 612 nm; Transmittance at 613 nm; Transmittance at 614 nm; Transmittance at 615 nm; Transmittance at 616 nm; Transmittance at 617 nm; Transmittance at 618 nm; Transmittance at 619 nm; Transmittance at 620 nm; Transmittance at 621 nm; Transmittance at 622 nm; Transmittance at 623 nm; Transmittance at 624 nm; Transmittance at 625 nm; Transmittance at 626 nm; Transmittance at

Type: Dataset

Format: text/tab-separated-values, 809621 data points

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106

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at station ALERT2018_13_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_13_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transmittance; Transmittance, photosynthetically active; Transmittance at 320 nm; Transmittance at 321 nm; Transmittance at 322 nm; Transmittance at 323 nm; Transmittance at 324 nm; Transmittance at 325 nm; Transmittance at 326 nm; Transmittance at 327 nm; Transmittance at 328 nm; Transmittance at 329 nm; Transmittance at 330 nm; Transmittance at 331 nm; Transmittance at 332 nm; Transmittance at 333 nm; Transmittance at 334 nm; Transmittance at 335 nm; Transmittance at 336 nm; Transmittance at 337 nm; Transmittance at 338 nm; Transmittance at 339 nm; Transmittance at 340 nm; Transmittance at 341 nm; Transmittance at 342 nm; Transmittance at 343 nm; Transmittance at 344 nm; Transmittance at 345 nm; Transmittance at 346 nm; Transmittance at 347 nm; Transmittance at 348 nm; Transmittance at 349 nm; Transmittance at 350 nm; Transmittance at 351 nm; Transmittance at 352 nm; Transmittance at 353 nm; Transmittance at 354 nm; Transmittance at 355 nm; Transmittance at 356 nm; Transmittance at 357 nm; Transmittance at 358 nm; Transmittance at 359 nm; Transmittance at 360 nm; Transmittance at 361 nm; Transmittance at 362 nm; Transmittance at 363 nm; Transmittance at 364 nm; Transmittance at 365 nm; Transmittance at 366 nm; Transmittance at 367 nm; Transmittance at 368 nm; Transmittance at 369 nm; Transmittance at 370 nm; Transmittance at 371 nm; Transmittance at 372 nm; Transmittance at 373 nm; Transmittance at 374 nm; Transmittance at 375 nm; Transmittance at 376 nm; Transmittance at 377 nm; Transmittance at 378 nm; Transmittance at 379 nm; Transmittance at 380 nm; Transmittance at 381 nm; Transmittance at 382 nm; Transmittance at 383 nm; Transmittance at 384 nm; Transmittance at 385 nm; Transmittance at 386 nm; Transmittance at 387 nm; Transmittance at 388 nm; Transmittance at 389 nm; Transmittance at 390 nm; Transmittance at 391 nm; Transmittance at 392 nm; Transmittance at 393 nm; Transmittance at 394 nm; Transmittance at 395 nm; Transmittance at 396 nm; Transmittance at 397 nm; Transmittance at 398 nm; Transmittance at 399 nm; Transmittance at 400 nm; Transmittance at 401 nm; Transmittance at 402 nm; Transmittance at 403 nm; Transmittance at 404 nm; Transmittance at 405 nm; Transmittance at 406 nm; Transmittance at 407 nm; Transmittance at 408 nm; Transmittance at 409 nm; Transmittance at 410 nm; Transmittance at 411 nm; Transmittance at 412 nm; Transmittance at 413 nm; Transmittance at 414 nm; Transmittance at 415 nm; Transmittance at 416 nm; Transmittance at 417 nm; Transmittance at 418 nm; Transmittance at 419 nm; Transmittance at 420 nm; Transmittance at 421 nm; Transmittance at 422 nm; Transmittance at 423 nm; Transmittance at 424 nm; Transmittance at 425 nm; Transmittance at 426 nm; Transmittance at 427 nm; Transmittance at 428 nm; Transmittance at 429 nm; Transmittance at 430 nm; Transmittance at 431 nm; Transmittance at 432 nm; Transmittance at 433 nm; Transmittance at 434 nm; Transmittance at 435 nm; Transmittance at 436 nm; Transmittance at 437 nm; Transmittance at 438 nm; Transmittance at 439 nm; Transmittance at 440 nm; Transmittance at 441 nm; Transmittance at 442 nm; Transmittance at 443 nm; Transmittance at 444 nm; Transmittance at 445 nm; Transmittance at 446 nm; Transmittance at 447 nm; Transmittance at 448 nm; Transmittance at 449 nm; Transmittance at 450 nm; Transmittance at 451 nm; Transmittance at 452 nm; Transmittance at 453 nm; Transmittance at 454 nm; Transmittance at 455 nm; Transmittance at 456 nm; Transmittance at 457 nm; Transmittance at 458 nm; Transmittance at 459 nm; Transmittance at 460 nm; Transmittance at 461 nm; Transmittance at 462 nm; Transmittance at 463 nm; Transmittance at 464 nm; Transmittance at 465 nm; Transmittance at 466 nm; Transmittance at 467 nm; Transmittance at 468 nm; Transmittance at 469 nm; Transmittance at 470 nm; Transmittance at 471 nm; Transmittance at 472 nm; Transmittance at 473 nm; Transmittance at 474 nm; Transmittance at 475 nm; Transmittance at 476 nm; Transmittance at 477 nm; Transmittance at 478 nm; Transmittance at 479 nm; Transmittance at 480 nm; Transmittance at 481 nm; Transmittance at 482 nm; Transmittance at 483 nm; Transmittance at 484 nm; Transmittance at 485 nm; Transmittance at 486 nm; Transmittance at 487 nm; Transmittance at 488 nm; Transmittance at 489 nm; Transmittance at 490 nm; Transmittance at 491 nm; Transmittance at 492 nm; Transmittance at 493 nm; Transmittance at 494 nm; Transmittance at 495 nm; Transmittance at 496 nm; Transmittance at 497 nm; Transmittance at 498 nm; Transmittance at 499 nm; Transmittance at 500 nm; Transmittance at 501 nm; Transmittance at 502 nm; Transmittance at 503 nm; Transmittance at 504 nm; Transmittance at 505 nm; Transmittance at 506 nm; Transmittance at 507 nm; Transmittance at 508 nm; Transmittance at 509 nm; Transmittance at 510 nm; Transmittance at 511 nm; Transmittance at 512 nm; Transmittance at 513 nm; Transmittance at 514 nm; Transmittance at 515 nm; Transmittance at 516 nm; Transmittance at 517 nm; Transmittance at 518 nm; Transmittance at 519 nm; Transmittance at 520 nm; Transmittance at 521 nm; Transmittance at 522 nm; Transmittance at 523 nm; Transmittance at 524 nm; Transmittance at 525 nm; Transmittance at 526 nm; Transmittance at 527 nm; Transmittance at 528 nm; Transmittance at 529 nm; Transmittance at 530 nm; Transmittance at 531 nm; Transmittance at 532 nm; Transmittance at 533 nm; Transmittance at 534 nm; Transmittance at 535 nm; Transmittance at 536 nm; Transmittance at 537 nm; Transmittance at 538 nm; Transmittance at 539 nm; Transmittance at 540 nm; Transmittance at 541 nm; Transmittance at 542 nm; Transmittance at 543 nm; Transmittance at 544 nm; Transmittance at 545 nm; Transmittance at 546 nm; Transmittance at 547 nm; Transmittance at 548 nm; Transmittance at 549 nm; Transmittance at 550 nm; Transmittance at 551 nm; Transmittance at 552 nm; Transmittance at 553 nm; Transmittance at 554 nm; Transmittance at 555 nm; Transmittance at 556 nm; Transmittance at 557 nm; Transmittance at 558 nm; Transmittance at 559 nm; Transmittance at 560 nm; Transmittance at 561 nm; Transmittance at 562 nm; Transmittance at 563 nm; Transmittance at 564 nm; Transmittance at 565 nm; Transmittance at 566 nm; Transmittance at 567 nm; Transmittance at 568 nm; Transmittance at 569 nm; Transmittance at 570 nm; Transmittance at 571 nm; Transmittance at 572 nm; Transmittance at 573 nm; Transmittance at 574 nm; Transmittance at 575 nm; Transmittance at 576 nm; Transmittance at 577 nm; Transmittance at 578 nm; Transmittance at 579 nm; Transmittance at 580 nm; Transmittance at 581 nm; Transmittance at 582 nm; Transmittance at 583 nm; Transmittance at 584 nm; Transmittance at 585 nm; Transmittance at 586 nm; Transmittance at 587 nm; Transmittance at 588 nm; Transmittance at 589 nm; Transmittance at 590 nm; Transmittance at 591 nm; Transmittance at 592 nm; Transmittance at 593 nm; Transmittance at 594 nm; Transmittance at 595 nm; Transmittance at 596 nm; Transmittance at 597 nm; Transmittance at 598 nm; Transmittance at 599 nm; Transmittance at 600 nm; Transmittance at 601 nm; Transmittance at 602 nm; Transmittance at 603 nm; Transmittance at 604 nm; Transmittance at 605 nm; Transmittance at 606 nm; Transmittance at 607 nm; Transmittance at 608 nm; Transmittance at 609 nm; Transmittance at 610 nm; Transmittance at 611 nm; Transmittance at 612 nm; Transmittance at 613 nm; Transmittance at 614 nm; Transmittance at 615 nm; Transmittance at 616 nm; Transmittance at 617 nm; Transmittance at 618 nm; Transmittance at 619 nm; Transmittance at 620 nm; Transmittance at 621 nm; Transmittance at 622 nm; Transmittance at 623 nm; Transmittance at 624 nm; Transmittance at 625 nm; Transmittance at 626 nm; Transmittance at

Type: Dataset

Format: text/tab-separated-values, 1362087 data points

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Fulltext

107

Unknown

Positioning of ROV at station ALERT2018_14_2 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_14_2; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Heading; LATITUDE; Lincoln Sea; LONGITUDE; Pitch angle; Remote operated vehicle; Roll angle; ROV; Sampling on land

Type: Dataset

Format: text/tab-separated-values, 1160 data points

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108

Unknown

Positioning of ROV at station ALERT2018_15_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_15_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Heading; LATITUDE; Lincoln Sea; LONGITUDE; Pitch angle; Remote operated vehicle; Roll angle; ROV; Sampling on land

Type: Dataset

Format: text/tab-separated-values, 89000 data points

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109

Unknown

Positioning of ROV at station ALERT2018_18_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_18_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Heading; LATITUDE; Lincoln Sea; LONGITUDE; Pitch angle; Remote operated vehicle; Roll angle; ROV; Sampling on land

Type: Dataset

Format: text/tab-separated-values, 98885 data points

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110

Unknown

Positioning of ROV at station ALERT2018_23_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_23_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Heading; LATITUDE; Lincoln Sea; LONGITUDE; Pitch angle; Remote operated vehicle; Roll angle; ROV; Sampling on land

Type: Dataset

Format: text/tab-separated-values, 98085 data points

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Fulltext

111

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at station ALERT2018_10_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_10_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transmittance; Transmittance, photosynthetically active; Transmittance at 320 nm; Transmittance at 321 nm; Transmittance at 322 nm; Transmittance at 323 nm; Transmittance at 324 nm; Transmittance at 325 nm; Transmittance at 326 nm; Transmittance at 327 nm; Transmittance at 328 nm; Transmittance at 329 nm; Transmittance at 330 nm; Transmittance at 331 nm; Transmittance at 332 nm; Transmittance at 333 nm; Transmittance at 334 nm; Transmittance at 335 nm; Transmittance at 336 nm; Transmittance at 337 nm; Transmittance at 338 nm; Transmittance at 339 nm; Transmittance at 340 nm; Transmittance at 341 nm; Transmittance at 342 nm; Transmittance at 343 nm; Transmittance at 344 nm; Transmittance at 345 nm; Transmittance at 346 nm; Transmittance at 347 nm; Transmittance at 348 nm; Transmittance at 349 nm; Transmittance at 350 nm; Transmittance at 351 nm; Transmittance at 352 nm; Transmittance at 353 nm; Transmittance at 354 nm; Transmittance at 355 nm; Transmittance at 356 nm; Transmittance at 357 nm; Transmittance at 358 nm; Transmittance at 359 nm; Transmittance at 360 nm; Transmittance at 361 nm; Transmittance at 362 nm; Transmittance at 363 nm; Transmittance at 364 nm; Transmittance at 365 nm; Transmittance at 366 nm; Transmittance at 367 nm; Transmittance at 368 nm; Transmittance at 369 nm; Transmittance at 370 nm; Transmittance at 371 nm; Transmittance at 372 nm; Transmittance at 373 nm; Transmittance at 374 nm; Transmittance at 375 nm; Transmittance at 376 nm; Transmittance at 377 nm; Transmittance at 378 nm; Transmittance at 379 nm; Transmittance at 380 nm; Transmittance at 381 nm; Transmittance at 382 nm; Transmittance at 383 nm; Transmittance at 384 nm; Transmittance at 385 nm; Transmittance at 386 nm; Transmittance at 387 nm; Transmittance at 388 nm; Transmittance at 389 nm; Transmittance at 390 nm; Transmittance at 391 nm; Transmittance at 392 nm; Transmittance at 393 nm; Transmittance at 394 nm; Transmittance at 395 nm; Transmittance at 396 nm; Transmittance at 397 nm; Transmittance at 398 nm; Transmittance at 399 nm; Transmittance at 400 nm; Transmittance at 401 nm; Transmittance at 402 nm; Transmittance at 403 nm; Transmittance at 404 nm; Transmittance at 405 nm; Transmittance at 406 nm; Transmittance at 407 nm; Transmittance at 408 nm; Transmittance at 409 nm; Transmittance at 410 nm; Transmittance at 411 nm; Transmittance at 412 nm; Transmittance at 413 nm; Transmittance at 414 nm; Transmittance at 415 nm; Transmittance at 416 nm; Transmittance at 417 nm; Transmittance at 418 nm; Transmittance at 419 nm; Transmittance at 420 nm; Transmittance at 421 nm; Transmittance at 422 nm; Transmittance at 423 nm; Transmittance at 424 nm; Transmittance at 425 nm; Transmittance at 426 nm; Transmittance at 427 nm; Transmittance at 428 nm; Transmittance at 429 nm; Transmittance at 430 nm; Transmittance at 431 nm; Transmittance at 432 nm; Transmittance at 433 nm; Transmittance at 434 nm; Transmittance at 435 nm; Transmittance at 436 nm; Transmittance at 437 nm; Transmittance at 438 nm; Transmittance at 439 nm; Transmittance at 440 nm; Transmittance at 441 nm; Transmittance at 442 nm; Transmittance at 443 nm; Transmittance at 444 nm; Transmittance at 445 nm; Transmittance at 446 nm; Transmittance at 447 nm; Transmittance at 448 nm; Transmittance at 449 nm; Transmittance at 450 nm; Transmittance at 451 nm; Transmittance at 452 nm; Transmittance at 453 nm; Transmittance at 454 nm; Transmittance at 455 nm; Transmittance at 456 nm; Transmittance at 457 nm; Transmittance at 458 nm; Transmittance at 459 nm; Transmittance at 460 nm; Transmittance at 461 nm; Transmittance at 462 nm; Transmittance at 463 nm; Transmittance at 464 nm; Transmittance at 465 nm; Transmittance at 466 nm; Transmittance at 467 nm; Transmittance at 468 nm; Transmittance at 469 nm; Transmittance at 470 nm; Transmittance at 471 nm; Transmittance at 472 nm; Transmittance at 473 nm; Transmittance at 474 nm; Transmittance at 475 nm; Transmittance at 476 nm; Transmittance at 477 nm; Transmittance at 478 nm; Transmittance at 479 nm; Transmittance at 480 nm; Transmittance at 481 nm; Transmittance at 482 nm; Transmittance at 483 nm; Transmittance at 484 nm; Transmittance at 485 nm; Transmittance at 486 nm; Transmittance at 487 nm; Transmittance at 488 nm; Transmittance at 489 nm; Transmittance at 490 nm; Transmittance at 491 nm; Transmittance at 492 nm; Transmittance at 493 nm; Transmittance at 494 nm; Transmittance at 495 nm; Transmittance at 496 nm; Transmittance at 497 nm; Transmittance at 498 nm; Transmittance at 499 nm; Transmittance at 500 nm; Transmittance at 501 nm; Transmittance at 502 nm; Transmittance at 503 nm; Transmittance at 504 nm; Transmittance at 505 nm; Transmittance at 506 nm; Transmittance at 507 nm; Transmittance at 508 nm; Transmittance at 509 nm; Transmittance at 510 nm; Transmittance at 511 nm; Transmittance at 512 nm; Transmittance at 513 nm; Transmittance at 514 nm; Transmittance at 515 nm; Transmittance at 516 nm; Transmittance at 517 nm; Transmittance at 518 nm; Transmittance at 519 nm; Transmittance at 520 nm; Transmittance at 521 nm; Transmittance at 522 nm; Transmittance at 523 nm; Transmittance at 524 nm; Transmittance at 525 nm; Transmittance at 526 nm; Transmittance at 527 nm; Transmittance at 528 nm; Transmittance at 529 nm; Transmittance at 530 nm; Transmittance at 531 nm; Transmittance at 532 nm; Transmittance at 533 nm; Transmittance at 534 nm; Transmittance at 535 nm; Transmittance at 536 nm; Transmittance at 537 nm; Transmittance at 538 nm; Transmittance at 539 nm; Transmittance at 540 nm; Transmittance at 541 nm; Transmittance at 542 nm; Transmittance at 543 nm; Transmittance at 544 nm; Transmittance at 545 nm; Transmittance at 546 nm; Transmittance at 547 nm; Transmittance at 548 nm; Transmittance at 549 nm; Transmittance at 550 nm; Transmittance at 551 nm; Transmittance at 552 nm; Transmittance at 553 nm; Transmittance at 554 nm; Transmittance at 555 nm; Transmittance at 556 nm; Transmittance at 557 nm; Transmittance at 558 nm; Transmittance at 559 nm; Transmittance at 560 nm; Transmittance at 561 nm; Transmittance at 562 nm; Transmittance at 563 nm; Transmittance at 564 nm; Transmittance at 565 nm; Transmittance at 566 nm; Transmittance at 567 nm; Transmittance at 568 nm; Transmittance at 569 nm; Transmittance at 570 nm; Transmittance at 571 nm; Transmittance at 572 nm; Transmittance at 573 nm; Transmittance at 574 nm; Transmittance at 575 nm; Transmittance at 576 nm; Transmittance at 577 nm; Transmittance at 578 nm; Transmittance at 579 nm; Transmittance at 580 nm; Transmittance at 581 nm; Transmittance at 582 nm; Transmittance at 583 nm; Transmittance at 584 nm; Transmittance at 585 nm; Transmittance at 586 nm; Transmittance at 587 nm; Transmittance at 588 nm; Transmittance at 589 nm; Transmittance at 590 nm; Transmittance at 591 nm; Transmittance at 592 nm; Transmittance at 593 nm; Transmittance at 594 nm; Transmittance at 595 nm; Transmittance at 596 nm; Transmittance at 597 nm; Transmittance at 598 nm; Transmittance at 599 nm; Transmittance at 600 nm; Transmittance at 601 nm; Transmittance at 602 nm; Transmittance at 603 nm; Transmittance at 604 nm; Transmittance at 605 nm; Transmittance at 606 nm; Transmittance at 607 nm; Transmittance at 608 nm; Transmittance at 609 nm; Transmittance at 610 nm; Transmittance at 611 nm; Transmittance at 612 nm; Transmittance at 613 nm; Transmittance at 614 nm; Transmittance at 615 nm; Transmittance at 616 nm; Transmittance at 617 nm; Transmittance at 618 nm; Transmittance at 619 nm; Transmittance at 620 nm; Transmittance at 621 nm; Transmittance at 622 nm; Transmittance at 623 nm; Transmittance at 624 nm; Transmittance at 625 nm; Transmittance at 626 nm; Transmittance at

Type: Dataset

Format: text/tab-separated-values, 2275137 data points

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S·F·X

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112

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at station ALERT2018_11_2 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_11_2; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transmittance; Transmittance, photosynthetically active; Transmittance at 320 nm; Transmittance at 321 nm; Transmittance at 322 nm; Transmittance at 323 nm; Transmittance at 324 nm; Transmittance at 325 nm; Transmittance at 326 nm; Transmittance at 327 nm; Transmittance at 328 nm; Transmittance at 329 nm; Transmittance at 330 nm; Transmittance at 331 nm; Transmittance at 332 nm; Transmittance at 333 nm; Transmittance at 334 nm; Transmittance at 335 nm; Transmittance at 336 nm; Transmittance at 337 nm; Transmittance at 338 nm; Transmittance at 339 nm; Transmittance at 340 nm; Transmittance at 341 nm; Transmittance at 342 nm; Transmittance at 343 nm; Transmittance at 344 nm; Transmittance at 345 nm; Transmittance at 346 nm; Transmittance at 347 nm; Transmittance at 348 nm; Transmittance at 349 nm; Transmittance at 350 nm; Transmittance at 351 nm; Transmittance at 352 nm; Transmittance at 353 nm; Transmittance at 354 nm; Transmittance at 355 nm; Transmittance at 356 nm; Transmittance at 357 nm; Transmittance at 358 nm; Transmittance at 359 nm; Transmittance at 360 nm; Transmittance at 361 nm; Transmittance at 362 nm; Transmittance at 363 nm; Transmittance at 364 nm; Transmittance at 365 nm; Transmittance at 366 nm; Transmittance at 367 nm; Transmittance at 368 nm; Transmittance at 369 nm; Transmittance at 370 nm; Transmittance at 371 nm; Transmittance at 372 nm; Transmittance at 373 nm; Transmittance at 374 nm; Transmittance at 375 nm; Transmittance at 376 nm; Transmittance at 377 nm; Transmittance at 378 nm; Transmittance at 379 nm; Transmittance at 380 nm; Transmittance at 381 nm; Transmittance at 382 nm; Transmittance at 383 nm; Transmittance at 384 nm; Transmittance at 385 nm; Transmittance at 386 nm; Transmittance at 387 nm; Transmittance at 388 nm; Transmittance at 389 nm; Transmittance at 390 nm; Transmittance at 391 nm; Transmittance at 392 nm; Transmittance at 393 nm; Transmittance at 394 nm; Transmittance at 395 nm; Transmittance at 396 nm; Transmittance at 397 nm; Transmittance at 398 nm; Transmittance at 399 nm; Transmittance at 400 nm; Transmittance at 401 nm; Transmittance at 402 nm; Transmittance at 403 nm; Transmittance at 404 nm; Transmittance at 405 nm; Transmittance at 406 nm; Transmittance at 407 nm; Transmittance at 408 nm; Transmittance at 409 nm; Transmittance at 410 nm; Transmittance at 411 nm; Transmittance at 412 nm; Transmittance at 413 nm; Transmittance at 414 nm; Transmittance at 415 nm; Transmittance at 416 nm; Transmittance at 417 nm; Transmittance at 418 nm; Transmittance at 419 nm; Transmittance at 420 nm; Transmittance at 421 nm; Transmittance at 422 nm; Transmittance at 423 nm; Transmittance at 424 nm; Transmittance at 425 nm; Transmittance at 426 nm; Transmittance at 427 nm; Transmittance at 428 nm; Transmittance at 429 nm; Transmittance at 430 nm; Transmittance at 431 nm; Transmittance at 432 nm; Transmittance at 433 nm; Transmittance at 434 nm; Transmittance at 435 nm; Transmittance at 436 nm; Transmittance at 437 nm; Transmittance at 438 nm; Transmittance at 439 nm; Transmittance at 440 nm; Transmittance at 441 nm; Transmittance at 442 nm; Transmittance at 443 nm; Transmittance at 444 nm; Transmittance at 445 nm; Transmittance at 446 nm; Transmittance at 447 nm; Transmittance at 448 nm; Transmittance at 449 nm; Transmittance at 450 nm; Transmittance at 451 nm; Transmittance at 452 nm; Transmittance at 453 nm; Transmittance at 454 nm; Transmittance at 455 nm; Transmittance at 456 nm; Transmittance at 457 nm; Transmittance at 458 nm; Transmittance at 459 nm; Transmittance at 460 nm; Transmittance at 461 nm; Transmittance at 462 nm; Transmittance at 463 nm; Transmittance at 464 nm; Transmittance at 465 nm; Transmittance at 466 nm; Transmittance at 467 nm; Transmittance at 468 nm; Transmittance at 469 nm; Transmittance at 470 nm; Transmittance at 471 nm; Transmittance at 472 nm; Transmittance at 473 nm; Transmittance at 474 nm; Transmittance at 475 nm; Transmittance at 476 nm; Transmittance at 477 nm; Transmittance at 478 nm; Transmittance at 479 nm; Transmittance at 480 nm; Transmittance at 481 nm; Transmittance at 482 nm; Transmittance at 483 nm; Transmittance at 484 nm; Transmittance at 485 nm; Transmittance at 486 nm; Transmittance at 487 nm; Transmittance at 488 nm; Transmittance at 489 nm; Transmittance at 490 nm; Transmittance at 491 nm; Transmittance at 492 nm; Transmittance at 493 nm; Transmittance at 494 nm; Transmittance at 495 nm; Transmittance at 496 nm; Transmittance at 497 nm; Transmittance at 498 nm; Transmittance at 499 nm; Transmittance at 500 nm; Transmittance at 501 nm; Transmittance at 502 nm; Transmittance at 503 nm; Transmittance at 504 nm; Transmittance at 505 nm; Transmittance at 506 nm; Transmittance at 507 nm; Transmittance at 508 nm; Transmittance at 509 nm; Transmittance at 510 nm; Transmittance at 511 nm; Transmittance at 512 nm; Transmittance at 513 nm; Transmittance at 514 nm; Transmittance at 515 nm; Transmittance at 516 nm; Transmittance at 517 nm; Transmittance at 518 nm; Transmittance at 519 nm; Transmittance at 520 nm; Transmittance at 521 nm; Transmittance at 522 nm; Transmittance at 523 nm; Transmittance at 524 nm; Transmittance at 525 nm; Transmittance at 526 nm; Transmittance at 527 nm; Transmittance at 528 nm; Transmittance at 529 nm; Transmittance at 530 nm; Transmittance at 531 nm; Transmittance at 532 nm; Transmittance at 533 nm; Transmittance at 534 nm; Transmittance at 535 nm; Transmittance at 536 nm; Transmittance at 537 nm; Transmittance at 538 nm; Transmittance at 539 nm; Transmittance at 540 nm; Transmittance at 541 nm; Transmittance at 542 nm; Transmittance at 543 nm; Transmittance at 544 nm; Transmittance at 545 nm; Transmittance at 546 nm; Transmittance at 547 nm; Transmittance at 548 nm; Transmittance at 549 nm; Transmittance at 550 nm; Transmittance at 551 nm; Transmittance at 552 nm; Transmittance at 553 nm; Transmittance at 554 nm; Transmittance at 555 nm; Transmittance at 556 nm; Transmittance at 557 nm; Transmittance at 558 nm; Transmittance at 559 nm; Transmittance at 560 nm; Transmittance at 561 nm; Transmittance at 562 nm; Transmittance at 563 nm; Transmittance at 564 nm; Transmittance at 565 nm; Transmittance at 566 nm; Transmittance at 567 nm; Transmittance at 568 nm; Transmittance at 569 nm; Transmittance at 570 nm; Transmittance at 571 nm; Transmittance at 572 nm; Transmittance at 573 nm; Transmittance at 574 nm; Transmittance at 575 nm; Transmittance at 576 nm; Transmittance at 577 nm; Transmittance at 578 nm; Transmittance at 579 nm; Transmittance at 580 nm; Transmittance at 581 nm; Transmittance at 582 nm; Transmittance at 583 nm; Transmittance at 584 nm; Transmittance at 585 nm; Transmittance at 586 nm; Transmittance at 587 nm; Transmittance at 588 nm; Transmittance at 589 nm; Transmittance at 590 nm; Transmittance at 591 nm; Transmittance at 592 nm; Transmittance at 593 nm; Transmittance at 594 nm; Transmittance at 595 nm; Transmittance at 596 nm; Transmittance at 597 nm; Transmittance at 598 nm; Transmittance at 599 nm; Transmittance at 600 nm; Transmittance at 601 nm; Transmittance at 602 nm; Transmittance at 603 nm; Transmittance at 604 nm; Transmittance at 605 nm; Transmittance at 606 nm; Transmittance at 607 nm; Transmittance at 608 nm; Transmittance at 609 nm; Transmittance at 610 nm; Transmittance at 611 nm; Transmittance at 612 nm; Transmittance at 613 nm; Transmittance at 614 nm; Transmittance at 615 nm; Transmittance at 616 nm; Transmittance at 617 nm; Transmittance at 618 nm; Transmittance at 619 nm; Transmittance at 620 nm; Transmittance at 621 nm; Transmittance at 622 nm; Transmittance at 623 nm; Transmittance at 624 nm; Transmittance at 625 nm; Transmittance at 626 nm; Transmittance at

Type: Dataset

Format: text/tab-separated-values, 1993900 data points

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S·F·X

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113

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at station ALERT2018_14_3 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_14_3; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transmittance; Transmittance, photosynthetically active; Transmittance at 320 nm; Transmittance at 321 nm; Transmittance at 322 nm; Transmittance at 323 nm; Transmittance at 324 nm; Transmittance at 325 nm; Transmittance at 326 nm; Transmittance at 327 nm; Transmittance at 328 nm; Transmittance at 329 nm; Transmittance at 330 nm; Transmittance at 331 nm; Transmittance at 332 nm; Transmittance at 333 nm; Transmittance at 334 nm; Transmittance at 335 nm; Transmittance at 336 nm; Transmittance at 337 nm; Transmittance at 338 nm; Transmittance at 339 nm; Transmittance at 340 nm; Transmittance at 341 nm; Transmittance at 342 nm; Transmittance at 343 nm; Transmittance at 344 nm; Transmittance at 345 nm; Transmittance at 346 nm; Transmittance at 347 nm; Transmittance at 348 nm; Transmittance at 349 nm; Transmittance at 350 nm; Transmittance at 351 nm; Transmittance at 352 nm; Transmittance at 353 nm; Transmittance at 354 nm; Transmittance at 355 nm; Transmittance at 356 nm; Transmittance at 357 nm; Transmittance at 358 nm; Transmittance at 359 nm; Transmittance at 360 nm; Transmittance at 361 nm; Transmittance at 362 nm; Transmittance at 363 nm; Transmittance at 364 nm; Transmittance at 365 nm; Transmittance at 366 nm; Transmittance at 367 nm; Transmittance at 368 nm; Transmittance at 369 nm; Transmittance at 370 nm; Transmittance at 371 nm; Transmittance at 372 nm; Transmittance at 373 nm; Transmittance at 374 nm; Transmittance at 375 nm; Transmittance at 376 nm; Transmittance at 377 nm; Transmittance at 378 nm; Transmittance at 379 nm; Transmittance at 380 nm; Transmittance at 381 nm; Transmittance at 382 nm; Transmittance at 383 nm; Transmittance at 384 nm; Transmittance at 385 nm; Transmittance at 386 nm; Transmittance at 387 nm; Transmittance at 388 nm; Transmittance at 389 nm; Transmittance at 390 nm; Transmittance at 391 nm; Transmittance at 392 nm; Transmittance at 393 nm; Transmittance at 394 nm; Transmittance at 395 nm; Transmittance at 396 nm; Transmittance at 397 nm; Transmittance at 398 nm; Transmittance at 399 nm; Transmittance at 400 nm; Transmittance at 401 nm; Transmittance at 402 nm; Transmittance at 403 nm; Transmittance at 404 nm; Transmittance at 405 nm; Transmittance at 406 nm; Transmittance at 407 nm; Transmittance at 408 nm; Transmittance at 409 nm; Transmittance at 410 nm; Transmittance at 411 nm; Transmittance at 412 nm; Transmittance at 413 nm; Transmittance at 414 nm; Transmittance at 415 nm; Transmittance at 416 nm; Transmittance at 417 nm; Transmittance at 418 nm; Transmittance at 419 nm; Transmittance at 420 nm; Transmittance at 421 nm; Transmittance at 422 nm; Transmittance at 423 nm; Transmittance at 424 nm; Transmittance at 425 nm; Transmittance at 426 nm; Transmittance at 427 nm; Transmittance at 428 nm; Transmittance at 429 nm; Transmittance at 430 nm; Transmittance at 431 nm; Transmittance at 432 nm; Transmittance at 433 nm; Transmittance at 434 nm; Transmittance at 435 nm; Transmittance at 436 nm; Transmittance at 437 nm; Transmittance at 438 nm; Transmittance at 439 nm; Transmittance at 440 nm; Transmittance at 441 nm; Transmittance at 442 nm; Transmittance at 443 nm; Transmittance at 444 nm; Transmittance at 445 nm; Transmittance at 446 nm; Transmittance at 447 nm; Transmittance at 448 nm; Transmittance at 449 nm; Transmittance at 450 nm; Transmittance at 451 nm; Transmittance at 452 nm; Transmittance at 453 nm; Transmittance at 454 nm; Transmittance at 455 nm; Transmittance at 456 nm; Transmittance at 457 nm; Transmittance at 458 nm; Transmittance at 459 nm; Transmittance at 460 nm; Transmittance at 461 nm; Transmittance at 462 nm; Transmittance at 463 nm; Transmittance at 464 nm; Transmittance at 465 nm; Transmittance at 466 nm; Transmittance at 467 nm; Transmittance at 468 nm; Transmittance at 469 nm; Transmittance at 470 nm; Transmittance at 471 nm; Transmittance at 472 nm; Transmittance at 473 nm; Transmittance at 474 nm; Transmittance at 475 nm; Transmittance at 476 nm; Transmittance at 477 nm; Transmittance at 478 nm; Transmittance at 479 nm; Transmittance at 480 nm; Transmittance at 481 nm; Transmittance at 482 nm; Transmittance at 483 nm; Transmittance at 484 nm; Transmittance at 485 nm; Transmittance at 486 nm; Transmittance at 487 nm; Transmittance at 488 nm; Transmittance at 489 nm; Transmittance at 490 nm; Transmittance at 491 nm; Transmittance at 492 nm; Transmittance at 493 nm; Transmittance at 494 nm; Transmittance at 495 nm; Transmittance at 496 nm; Transmittance at 497 nm; Transmittance at 498 nm; Transmittance at 499 nm; Transmittance at 500 nm; Transmittance at 501 nm; Transmittance at 502 nm; Transmittance at 503 nm; Transmittance at 504 nm; Transmittance at 505 nm; Transmittance at 506 nm; Transmittance at 507 nm; Transmittance at 508 nm; Transmittance at 509 nm; Transmittance at 510 nm; Transmittance at 511 nm; Transmittance at 512 nm; Transmittance at 513 nm; Transmittance at 514 nm; Transmittance at 515 nm; Transmittance at 516 nm; Transmittance at 517 nm; Transmittance at 518 nm; Transmittance at 519 nm; Transmittance at 520 nm; Transmittance at 521 nm; Transmittance at 522 nm; Transmittance at 523 nm; Transmittance at 524 nm; Transmittance at 525 nm; Transmittance at 526 nm; Transmittance at 527 nm; Transmittance at 528 nm; Transmittance at 529 nm; Transmittance at 530 nm; Transmittance at 531 nm; Transmittance at 532 nm; Transmittance at 533 nm; Transmittance at 534 nm; Transmittance at 535 nm; Transmittance at 536 nm; Transmittance at 537 nm; Transmittance at 538 nm; Transmittance at 539 nm; Transmittance at 540 nm; Transmittance at 541 nm; Transmittance at 542 nm; Transmittance at 543 nm; Transmittance at 544 nm; Transmittance at 545 nm; Transmittance at 546 nm; Transmittance at 547 nm; Transmittance at 548 nm; Transmittance at 549 nm; Transmittance at 550 nm; Transmittance at 551 nm; Transmittance at 552 nm; Transmittance at 553 nm; Transmittance at 554 nm; Transmittance at 555 nm; Transmittance at 556 nm; Transmittance at 557 nm; Transmittance at 558 nm; Transmittance at 559 nm; Transmittance at 560 nm; Transmittance at 561 nm; Transmittance at 562 nm; Transmittance at 563 nm; Transmittance at 564 nm; Transmittance at 565 nm; Transmittance at 566 nm; Transmittance at 567 nm; Transmittance at 568 nm; Transmittance at 569 nm; Transmittance at 570 nm; Transmittance at 571 nm; Transmittance at 572 nm; Transmittance at 573 nm; Transmittance at 574 nm; Transmittance at 575 nm; Transmittance at 576 nm; Transmittance at 577 nm; Transmittance at 578 nm; Transmittance at 579 nm; Transmittance at 580 nm; Transmittance at 581 nm; Transmittance at 582 nm; Transmittance at 583 nm; Transmittance at 584 nm; Transmittance at 585 nm; Transmittance at 586 nm; Transmittance at 587 nm; Transmittance at 588 nm; Transmittance at 589 nm; Transmittance at 590 nm; Transmittance at 591 nm; Transmittance at 592 nm; Transmittance at 593 nm; Transmittance at 594 nm; Transmittance at 595 nm; Transmittance at 596 nm; Transmittance at 597 nm; Transmittance at 598 nm; Transmittance at 599 nm; Transmittance at 600 nm; Transmittance at 601 nm; Transmittance at 602 nm; Transmittance at 603 nm; Transmittance at 604 nm; Transmittance at 605 nm; Transmittance at 606 nm; Transmittance at 607 nm; Transmittance at 608 nm; Transmittance at 609 nm; Transmittance at 610 nm; Transmittance at 611 nm; Transmittance at 612 nm; Transmittance at 613 nm; Transmittance at 614 nm; Transmittance at 615 nm; Transmittance at 616 nm; Transmittance at 617 nm; Transmittance at 618 nm; Transmittance at 619 nm; Transmittance at 620 nm; Transmittance at 621 nm; Transmittance at 622 nm; Transmittance at 623 nm; Transmittance at 624 nm; Transmittance at 625 nm; Transmittance at 626 nm; Transmittance at

Type: Dataset

Format: text/tab-separated-values, 408151 data points

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S·F·X

Fulltext

114

Unknown

Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at station ALERT2018_15_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_15_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transmittance; Transmittance, photosynthetically active; Transmittance at 320 nm; Transmittance at 321 nm; Transmittance at 322 nm; Transmittance at 323 nm; Transmittance at 324 nm; Transmittance at 325 nm; Transmittance at 326 nm; Transmittance at 327 nm; Transmittance at 328 nm; Transmittance at 329 nm; Transmittance at 330 nm; Transmittance at 331 nm; Transmittance at 332 nm; Transmittance at 333 nm; Transmittance at 334 nm; Transmittance at 335 nm; Transmittance at 336 nm; Transmittance at 337 nm; Transmittance at 338 nm; Transmittance at 339 nm; Transmittance at 340 nm; Transmittance at 341 nm; Transmittance at 342 nm; Transmittance at 343 nm; Transmittance at 344 nm; Transmittance at 345 nm; Transmittance at 346 nm; Transmittance at 347 nm; Transmittance at 348 nm; Transmittance at 349 nm; Transmittance at 350 nm; Transmittance at 351 nm; Transmittance at 352 nm; Transmittance at 353 nm; Transmittance at 354 nm; Transmittance at 355 nm; Transmittance at 356 nm; Transmittance at 357 nm; Transmittance at 358 nm; Transmittance at 359 nm; Transmittance at 360 nm; Transmittance at 361 nm; Transmittance at 362 nm; Transmittance at 363 nm; Transmittance at 364 nm; Transmittance at 365 nm; Transmittance at 366 nm; Transmittance at 367 nm; Transmittance at 368 nm; Transmittance at 369 nm; Transmittance at 370 nm; Transmittance at 371 nm; Transmittance at 372 nm; Transmittance at 373 nm; Transmittance at 374 nm; Transmittance at 375 nm; Transmittance at 376 nm; Transmittance at 377 nm; Transmittance at 378 nm; Transmittance at 379 nm; Transmittance at 380 nm; Transmittance at 381 nm; Transmittance at 382 nm; Transmittance at 383 nm; Transmittance at 384 nm; Transmittance at 385 nm; Transmittance at 386 nm; Transmittance at 387 nm; Transmittance at 388 nm; Transmittance at 389 nm; Transmittance at 390 nm; Transmittance at 391 nm; Transmittance at 392 nm; Transmittance at 393 nm; Transmittance at 394 nm; Transmittance at 395 nm; Transmittance at 396 nm; Transmittance at 397 nm; Transmittance at 398 nm; Transmittance at 399 nm; Transmittance at 400 nm; Transmittance at 401 nm; Transmittance at 402 nm; Transmittance at 403 nm; Transmittance at 404 nm; Transmittance at 405 nm; Transmittance at 406 nm; Transmittance at 407 nm; Transmittance at 408 nm; Transmittance at 409 nm; Transmittance at 410 nm; Transmittance at 411 nm; Transmittance at 412 nm; Transmittance at 413 nm; Transmittance at 414 nm; Transmittance at 415 nm; Transmittance at 416 nm; Transmittance at 417 nm; Transmittance at 418 nm; Transmittance at 419 nm; Transmittance at 420 nm; Transmittance at 421 nm; Transmittance at 422 nm; Transmittance at 423 nm; Transmittance at 424 nm; Transmittance at 425 nm; Transmittance at 426 nm; Transmittance at 427 nm; Transmittance at 428 nm; Transmittance at 429 nm; Transmittance at 430 nm; Transmittance at 431 nm; Transmittance at 432 nm; Transmittance at 433 nm; Transmittance at 434 nm; Transmittance at 435 nm; Transmittance at 436 nm; Transmittance at 437 nm; Transmittance at 438 nm; Transmittance at 439 nm; Transmittance at 440 nm; Transmittance at 441 nm; Transmittance at 442 nm; Transmittance at 443 nm; Transmittance at 444 nm; Transmittance at 445 nm; Transmittance at 446 nm; Transmittance at 447 nm; Transmittance at 448 nm; Transmittance at 449 nm; Transmittance at 450 nm; Transmittance at 451 nm; Transmittance at 452 nm; Transmittance at 453 nm; Transmittance at 454 nm; Transmittance at 455 nm; Transmittance at 456 nm; Transmittance at 457 nm; Transmittance at 458 nm; Transmittance at 459 nm; Transmittance at 460 nm; Transmittance at 461 nm; Transmittance at 462 nm; Transmittance at 463 nm; Transmittance at 464 nm; Transmittance at 465 nm; Transmittance at 466 nm; Transmittance at 467 nm; Transmittance at 468 nm; Transmittance at 469 nm; Transmittance at 470 nm; Transmittance at 471 nm; Transmittance at 472 nm; Transmittance at 473 nm; Transmittance at 474 nm; Transmittance at 475 nm; Transmittance at 476 nm; Transmittance at 477 nm; Transmittance at 478 nm; Transmittance at 479 nm; Transmittance at 480 nm; Transmittance at 481 nm; Transmittance at 482 nm; Transmittance at 483 nm; Transmittance at 484 nm; Transmittance at 485 nm; Transmittance at 486 nm; Transmittance at 487 nm; Transmittance at 488 nm; Transmittance at 489 nm; Transmittance at 490 nm; Transmittance at 491 nm; Transmittance at 492 nm; Transmittance at 493 nm; Transmittance at 494 nm; Transmittance at 495 nm; Transmittance at 496 nm; Transmittance at 497 nm; Transmittance at 498 nm; Transmittance at 499 nm; Transmittance at 500 nm; Transmittance at 501 nm; Transmittance at 502 nm; Transmittance at 503 nm; Transmittance at 504 nm; Transmittance at 505 nm; Transmittance at 506 nm; Transmittance at 507 nm; Transmittance at 508 nm; Transmittance at 509 nm; Transmittance at 510 nm; Transmittance at 511 nm; Transmittance at 512 nm; Transmittance at 513 nm; Transmittance at 514 nm; Transmittance at 515 nm; Transmittance at 516 nm; Transmittance at 517 nm; Transmittance at 518 nm; Transmittance at 519 nm; Transmittance at 520 nm; Transmittance at 521 nm; Transmittance at 522 nm; Transmittance at 523 nm; Transmittance at 524 nm; Transmittance at 525 nm; Transmittance at 526 nm; Transmittance at 527 nm; Transmittance at 528 nm; Transmittance at 529 nm; Transmittance at 530 nm; Transmittance at 531 nm; Transmittance at 532 nm; Transmittance at 533 nm; Transmittance at 534 nm; Transmittance at 535 nm; Transmittance at 536 nm; Transmittance at 537 nm; Transmittance at 538 nm; Transmittance at 539 nm; Transmittance at 540 nm; Transmittance at 541 nm; Transmittance at 542 nm; Transmittance at 543 nm; Transmittance at 544 nm; Transmittance at 545 nm; Transmittance at 546 nm; Transmittance at 547 nm; Transmittance at 548 nm; Transmittance at 549 nm; Transmittance at 550 nm; Transmittance at 551 nm; Transmittance at 552 nm; Transmittance at 553 nm; Transmittance at 554 nm; Transmittance at 555 nm; Transmittance at 556 nm; Transmittance at 557 nm; Transmittance at 558 nm; Transmittance at 559 nm; Transmittance at 560 nm; Transmittance at 561 nm; Transmittance at 562 nm; Transmittance at 563 nm; Transmittance at 564 nm; Transmittance at 565 nm; Transmittance at 566 nm; Transmittance at 567 nm; Transmittance at 568 nm; Transmittance at 569 nm; Transmittance at 570 nm; Transmittance at 571 nm; Transmittance at 572 nm; Transmittance at 573 nm; Transmittance at 574 nm; Transmittance at 575 nm; Transmittance at 576 nm; Transmittance at 577 nm; Transmittance at 578 nm; Transmittance at 579 nm; Transmittance at 580 nm; Transmittance at 581 nm; Transmittance at 582 nm; Transmittance at 583 nm; Transmittance at 584 nm; Transmittance at 585 nm; Transmittance at 586 nm; Transmittance at 587 nm; Transmittance at 588 nm; Transmittance at 589 nm; Transmittance at 590 nm; Transmittance at 591 nm; Transmittance at 592 nm; Transmittance at 593 nm; Transmittance at 594 nm; Transmittance at 595 nm; Transmittance at 596 nm; Transmittance at 597 nm; Transmittance at 598 nm; Transmittance at 599 nm; Transmittance at 600 nm; Transmittance at 601 nm; Transmittance at 602 nm; Transmittance at 603 nm; Transmittance at 604 nm; Transmittance at 605 nm; Transmittance at 606 nm; Transmittance at 607 nm; Transmittance at 608 nm; Transmittance at 609 nm; Transmittance at 610 nm; Transmittance at 611 nm; Transmittance at 612 nm; Transmittance at 613 nm; Transmittance at 614 nm; Transmittance at 615 nm; Transmittance at 616 nm; Transmittance at 617 nm; Transmittance at 618 nm; Transmittance at 619 nm; Transmittance at 620 nm; Transmittance at 621 nm; Transmittance at 622 nm; Transmittance at 623 nm; Transmittance at 624 nm; Transmittance at 625 nm; Transmittance at 626 nm; Transmittance at

Type: Dataset

Format: text/tab-separated-values, 1901411 data points

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S·F·X

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115

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Fraction of spectral solar irradiance transmitted through snow and sea ice as measured in different depths under sea ice (transmittance) at station ALERT2018_19_2 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_19_2; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transmittance; Transmittance, photosynthetically active; Transmittance at 320 nm; Transmittance at 321 nm; Transmittance at 322 nm; Transmittance at 323 nm; Transmittance at 324 nm; Transmittance at 325 nm; Transmittance at 326 nm; Transmittance at 327 nm; Transmittance at 328 nm; Transmittance at 329 nm; Transmittance at 330 nm; Transmittance at 331 nm; Transmittance at 332 nm; Transmittance at 333 nm; Transmittance at 334 nm; Transmittance at 335 nm; Transmittance at 336 nm; Transmittance at 337 nm; Transmittance at 338 nm; Transmittance at 339 nm; Transmittance at 340 nm; Transmittance at 341 nm; Transmittance at 342 nm; Transmittance at 343 nm; Transmittance at 344 nm; Transmittance at 345 nm; Transmittance at 346 nm; Transmittance at 347 nm; Transmittance at 348 nm; Transmittance at 349 nm; Transmittance at 350 nm; Transmittance at 351 nm; Transmittance at 352 nm; Transmittance at 353 nm; Transmittance at 354 nm; Transmittance at 355 nm; Transmittance at 356 nm; Transmittance at 357 nm; Transmittance at 358 nm; Transmittance at 359 nm; Transmittance at 360 nm; Transmittance at 361 nm; Transmittance at 362 nm; Transmittance at 363 nm; Transmittance at 364 nm; Transmittance at 365 nm; Transmittance at 366 nm; Transmittance at 367 nm; Transmittance at 368 nm; Transmittance at 369 nm; Transmittance at 370 nm; Transmittance at 371 nm; Transmittance at 372 nm; Transmittance at 373 nm; Transmittance at 374 nm; Transmittance at 375 nm; Transmittance at 376 nm; Transmittance at 377 nm; Transmittance at 378 nm; Transmittance at 379 nm; Transmittance at 380 nm; Transmittance at 381 nm; Transmittance at 382 nm; Transmittance at 383 nm; Transmittance at 384 nm; Transmittance at 385 nm; Transmittance at 386 nm; Transmittance at 387 nm; Transmittance at 388 nm; Transmittance at 389 nm; Transmittance at 390 nm; Transmittance at 391 nm; Transmittance at 392 nm; Transmittance at 393 nm; Transmittance at 394 nm; Transmittance at 395 nm; Transmittance at 396 nm; Transmittance at 397 nm; Transmittance at 398 nm; Transmittance at 399 nm; Transmittance at 400 nm; Transmittance at 401 nm; Transmittance at 402 nm; Transmittance at 403 nm; Transmittance at 404 nm; Transmittance at 405 nm; Transmittance at 406 nm; Transmittance at 407 nm; Transmittance at 408 nm; Transmittance at 409 nm; Transmittance at 410 nm; Transmittance at 411 nm; Transmittance at 412 nm; Transmittance at 413 nm; Transmittance at 414 nm; Transmittance at 415 nm; Transmittance at 416 nm; Transmittance at 417 nm; Transmittance at 418 nm; Transmittance at 419 nm; Transmittance at 420 nm; Transmittance at 421 nm; Transmittance at 422 nm; Transmittance at 423 nm; Transmittance at 424 nm; Transmittance at 425 nm; Transmittance at 426 nm; Transmittance at 427 nm; Transmittance at 428 nm; Transmittance at 429 nm; Transmittance at 430 nm; Transmittance at 431 nm; Transmittance at 432 nm; Transmittance at 433 nm; Transmittance at 434 nm; Transmittance at 435 nm; Transmittance at 436 nm; Transmittance at 437 nm; Transmittance at 438 nm; Transmittance at 439 nm; Transmittance at 440 nm; Transmittance at 441 nm; Transmittance at 442 nm; Transmittance at 443 nm; Transmittance at 444 nm; Transmittance at 445 nm; Transmittance at 446 nm; Transmittance at 447 nm; Transmittance at 448 nm; Transmittance at 449 nm; Transmittance at 450 nm; Transmittance at 451 nm; Transmittance at 452 nm; Transmittance at 453 nm; Transmittance at 454 nm; Transmittance at 455 nm; Transmittance at 456 nm; Transmittance at 457 nm; Transmittance at 458 nm; Transmittance at 459 nm; Transmittance at 460 nm; Transmittance at 461 nm; Transmittance at 462 nm; Transmittance at 463 nm; Transmittance at 464 nm; Transmittance at 465 nm; Transmittance at 466 nm; Transmittance at 467 nm; Transmittance at 468 nm; Transmittance at 469 nm; Transmittance at 470 nm; Transmittance at 471 nm; Transmittance at 472 nm; Transmittance at 473 nm; Transmittance at 474 nm; Transmittance at 475 nm; Transmittance at 476 nm; Transmittance at 477 nm; Transmittance at 478 nm; Transmittance at 479 nm; Transmittance at 480 nm; Transmittance at 481 nm; Transmittance at 482 nm; Transmittance at 483 nm; Transmittance at 484 nm; Transmittance at 485 nm; Transmittance at 486 nm; Transmittance at 487 nm; Transmittance at 488 nm; Transmittance at 489 nm; Transmittance at 490 nm; Transmittance at 491 nm; Transmittance at 492 nm; Transmittance at 493 nm; Transmittance at 494 nm; Transmittance at 495 nm; Transmittance at 496 nm; Transmittance at 497 nm; Transmittance at 498 nm; Transmittance at 499 nm; Transmittance at 500 nm; Transmittance at 501 nm; Transmittance at 502 nm; Transmittance at 503 nm; Transmittance at 504 nm; Transmittance at 505 nm; Transmittance at 506 nm; Transmittance at 507 nm; Transmittance at 508 nm; Transmittance at 509 nm; Transmittance at 510 nm; Transmittance at 511 nm; Transmittance at 512 nm; Transmittance at 513 nm; Transmittance at 514 nm; Transmittance at 515 nm; Transmittance at 516 nm; Transmittance at 517 nm; Transmittance at 518 nm; Transmittance at 519 nm; Transmittance at 520 nm; Transmittance at 521 nm; Transmittance at 522 nm; Transmittance at 523 nm; Transmittance at 524 nm; Transmittance at 525 nm; Transmittance at 526 nm; Transmittance at 527 nm; Transmittance at 528 nm; Transmittance at 529 nm; Transmittance at 530 nm; Transmittance at 531 nm; Transmittance at 532 nm; Transmittance at 533 nm; Transmittance at 534 nm; Transmittance at 535 nm; Transmittance at 536 nm; Transmittance at 537 nm; Transmittance at 538 nm; Transmittance at 539 nm; Transmittance at 540 nm; Transmittance at 541 nm; Transmittance at 542 nm; Transmittance at 543 nm; Transmittance at 544 nm; Transmittance at 545 nm; Transmittance at 546 nm; Transmittance at 547 nm; Transmittance at 548 nm; Transmittance at 549 nm; Transmittance at 550 nm; Transmittance at 551 nm; Transmittance at 552 nm; Transmittance at 553 nm; Transmittance at 554 nm; Transmittance at 555 nm; Transmittance at 556 nm; Transmittance at 557 nm; Transmittance at 558 nm; Transmittance at 559 nm; Transmittance at 560 nm; Transmittance at 561 nm; Transmittance at 562 nm; Transmittance at 563 nm; Transmittance at 564 nm; Transmittance at 565 nm; Transmittance at 566 nm; Transmittance at 567 nm; Transmittance at 568 nm; Transmittance at 569 nm; Transmittance at 570 nm; Transmittance at 571 nm; Transmittance at 572 nm; Transmittance at 573 nm; Transmittance at 574 nm; Transmittance at 575 nm; Transmittance at 576 nm; Transmittance at 577 nm; Transmittance at 578 nm; Transmittance at 579 nm; Transmittance at 580 nm; Transmittance at 581 nm; Transmittance at 582 nm; Transmittance at 583 nm; Transmittance at 584 nm; Transmittance at 585 nm; Transmittance at 586 nm; Transmittance at 587 nm; Transmittance at 588 nm; Transmittance at 589 nm; Transmittance at 590 nm; Transmittance at 591 nm; Transmittance at 592 nm; Transmittance at 593 nm; Transmittance at 594 nm; Transmittance at 595 nm; Transmittance at 596 nm; Transmittance at 597 nm; Transmittance at 598 nm; Transmittance at 599 nm; Transmittance at 600 nm; Transmittance at 601 nm; Transmittance at 602 nm; Transmittance at 603 nm; Transmittance at 604 nm; Transmittance at 605 nm; Transmittance at 606 nm; Transmittance at 607 nm; Transmittance at 608 nm; Transmittance at 609 nm; Transmittance at 610 nm; Transmittance at 611 nm; Transmittance at 612 nm; Transmittance at 613 nm; Transmittance at 614 nm; Transmittance at 615 nm; Transmittance at 616 nm; Transmittance at 617 nm; Transmittance at 618 nm; Transmittance at 619 nm; Transmittance at 620 nm; Transmittance at 621 nm; Transmittance at 622 nm; Transmittance at 623 nm; Transmittance at 624 nm; Transmittance at 625 nm; Transmittance at 626 nm; Transmittance at

Type: Dataset

Format: text/tab-separated-values, 1957851 data points

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S·F·X

Fulltext

116

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Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at station ALERT2018_08_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_08_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transflectance; Transflectance, photosynthetically active; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615

Type: Dataset

Format: text/tab-separated-values, 522605 data points

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S·F·X

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117

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Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at station ALERT2018_11_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_11_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transflectance; Transflectance, photosynthetically active; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615

Type: Dataset

Format: text/tab-separated-values, 1609090 data points

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S·F·X

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Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at station ALERT2018_13_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_13_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transflectance; Transflectance, photosynthetically active; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615

Type: Dataset

Format: text/tab-separated-values, 1669317 data points

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DATA PANGAEA

S·F·X

Fulltext

119

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Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at station ALERT2018_14_1 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_14_1; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transflectance; Transflectance, photosynthetically active; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615

Type: Dataset

Format: text/tab-separated-values, 3924935 data points

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S·F·X

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120

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Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at station ALERT2018_14_3 (2019)

Anhaus, Philipp ; Katlein, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Details

Publication Date: 2023-03-16

Keywords: ALERT2018; ALERT2018_14_3; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; Hyperspectral radiometer, TriOS Mess- und Datentechnik GmbH, RAMSES; LATITUDE; Lincoln Sea; LONGITUDE; Remote operated vehicle; ROV; Sampling on land; Transflectance; Transflectance, photosynthetically active; Transflectance at 320 nm; Transflectance at 321 nm; Transflectance at 322 nm; Transflectance at 323 nm; Transflectance at 324 nm; Transflectance at 325 nm; Transflectance at 326 nm; Transflectance at 327 nm; Transflectance at 328 nm; Transflectance at 329 nm; Transflectance at 330 nm; Transflectance at 331 nm; Transflectance at 332 nm; Transflectance at 333 nm; Transflectance at 334 nm; Transflectance at 335 nm; Transflectance at 336 nm; Transflectance at 337 nm; Transflectance at 338 nm; Transflectance at 339 nm; Transflectance at 340 nm; Transflectance at 341 nm; Transflectance at 342 nm; Transflectance at 343 nm; Transflectance at 344 nm; Transflectance at 345 nm; Transflectance at 346 nm; Transflectance at 347 nm; Transflectance at 348 nm; Transflectance at 349 nm; Transflectance at 350 nm; Transflectance at 351 nm; Transflectance at 352 nm; Transflectance at 353 nm; Transflectance at 354 nm; Transflectance at 355 nm; Transflectance at 356 nm; Transflectance at 357 nm; Transflectance at 358 nm; Transflectance at 359 nm; Transflectance at 360 nm; Transflectance at 361 nm; Transflectance at 362 nm; Transflectance at 363 nm; Transflectance at 364 nm; Transflectance at 365 nm; Transflectance at 366 nm; Transflectance at 367 nm; Transflectance at 368 nm; Transflectance at 369 nm; Transflectance at 370 nm; Transflectance at 371 nm; Transflectance at 372 nm; Transflectance at 373 nm; Transflectance at 374 nm; Transflectance at 375 nm; Transflectance at 376 nm; Transflectance at 377 nm; Transflectance at 378 nm; Transflectance at 379 nm; Transflectance at 380 nm; Transflectance at 381 nm; Transflectance at 382 nm; Transflectance at 383 nm; Transflectance at 384 nm; Transflectance at 385 nm; Transflectance at 386 nm; Transflectance at 387 nm; Transflectance at 388 nm; Transflectance at 389 nm; Transflectance at 390 nm; Transflectance at 391 nm; Transflectance at 392 nm; Transflectance at 393 nm; Transflectance at 394 nm; Transflectance at 395 nm; Transflectance at 396 nm; Transflectance at 397 nm; Transflectance at 398 nm; Transflectance at 399 nm; Transflectance at 400 nm; Transflectance at 401 nm; Transflectance at 402 nm; Transflectance at 403 nm; Transflectance at 404 nm; Transflectance at 405 nm; Transflectance at 406 nm; Transflectance at 407 nm; Transflectance at 408 nm; Transflectance at 409 nm; Transflectance at 410 nm; Transflectance at 411 nm; Transflectance at 412 nm; Transflectance at 413 nm; Transflectance at 414 nm; Transflectance at 415 nm; Transflectance at 416 nm; Transflectance at 417 nm; Transflectance at 418 nm; Transflectance at 419 nm; Transflectance at 420 nm; Transflectance at 421 nm; Transflectance at 422 nm; Transflectance at 423 nm; Transflectance at 424 nm; Transflectance at 425 nm; Transflectance at 426 nm; Transflectance at 427 nm; Transflectance at 428 nm; Transflectance at 429 nm; Transflectance at 430 nm; Transflectance at 431 nm; Transflectance at 432 nm; Transflectance at 433 nm; Transflectance at 434 nm; Transflectance at 435 nm; Transflectance at 436 nm; Transflectance at 437 nm; Transflectance at 438 nm; Transflectance at 439 nm; Transflectance at 440 nm; Transflectance at 441 nm; Transflectance at 442 nm; Transflectance at 443 nm; Transflectance at 444 nm; Transflectance at 445 nm; Transflectance at 446 nm; Transflectance at 447 nm; Transflectance at 448 nm; Transflectance at 449 nm; Transflectance at 450 nm; Transflectance at 451 nm; Transflectance at 452 nm; Transflectance at 453 nm; Transflectance at 454 nm; Transflectance at 455 nm; Transflectance at 456 nm; Transflectance at 457 nm; Transflectance at 458 nm; Transflectance at 459 nm; Transflectance at 460 nm; Transflectance at 461 nm; Transflectance at 462 nm; Transflectance at 463 nm; Transflectance at 464 nm; Transflectance at 465 nm; Transflectance at 466 nm; Transflectance at 467 nm; Transflectance at 468 nm; Transflectance at 469 nm; Transflectance at 470 nm; Transflectance at 471 nm; Transflectance at 472 nm; Transflectance at 473 nm; Transflectance at 474 nm; Transflectance at 475 nm; Transflectance at 476 nm; Transflectance at 477 nm; Transflectance at 478 nm; Transflectance at 479 nm; Transflectance at 480 nm; Transflectance at 481 nm; Transflectance at 482 nm; Transflectance at 483 nm; Transflectance at 484 nm; Transflectance at 485 nm; Transflectance at 486 nm; Transflectance at 487 nm; Transflectance at 488 nm; Transflectance at 489 nm; Transflectance at 490 nm; Transflectance at 491 nm; Transflectance at 492 nm; Transflectance at 493 nm; Transflectance at 494 nm; Transflectance at 495 nm; Transflectance at 496 nm; Transflectance at 497 nm; Transflectance at 498 nm; Transflectance at 499 nm; Transflectance at 500 nm; Transflectance at 501 nm; Transflectance at 502 nm; Transflectance at 503 nm; Transflectance at 504 nm; Transflectance at 505 nm; Transflectance at 506 nm; Transflectance at 507 nm; Transflectance at 508 nm; Transflectance at 509 nm; Transflectance at 510 nm; Transflectance at 511 nm; Transflectance at 512 nm; Transflectance at 513 nm; Transflectance at 514 nm; Transflectance at 515 nm; Transflectance at 516 nm; Transflectance at 517 nm; Transflectance at 518 nm; Transflectance at 519 nm; Transflectance at 520 nm; Transflectance at 521 nm; Transflectance at 522 nm; Transflectance at 523 nm; Transflectance at 524 nm; Transflectance at 525 nm; Transflectance at 526 nm; Transflectance at 527 nm; Transflectance at 528 nm; Transflectance at 529 nm; Transflectance at 530 nm; Transflectance at 531 nm; Transflectance at 532 nm; Transflectance at 533 nm; Transflectance at 534 nm; Transflectance at 535 nm; Transflectance at 536 nm; Transflectance at 537 nm; Transflectance at 538 nm; Transflectance at 539 nm; Transflectance at 540 nm; Transflectance at 541 nm; Transflectance at 542 nm; Transflectance at 543 nm; Transflectance at 544 nm; Transflectance at 545 nm; Transflectance at 546 nm; Transflectance at 547 nm; Transflectance at 548 nm; Transflectance at 549 nm; Transflectance at 550 nm; Transflectance at 551 nm; Transflectance at 552 nm; Transflectance at 553 nm; Transflectance at 554 nm; Transflectance at 555 nm; Transflectance at 556 nm; Transflectance at 557 nm; Transflectance at 558 nm; Transflectance at 559 nm; Transflectance at 560 nm; Transflectance at 561 nm; Transflectance at 562 nm; Transflectance at 563 nm; Transflectance at 564 nm; Transflectance at 565 nm; Transflectance at 566 nm; Transflectance at 567 nm; Transflectance at 568 nm; Transflectance at 569 nm; Transflectance at 570 nm; Transflectance at 571 nm; Transflectance at 572 nm; Transflectance at 573 nm; Transflectance at 574 nm; Transflectance at 575 nm; Transflectance at 576 nm; Transflectance at 577 nm; Transflectance at 578 nm; Transflectance at 579 nm; Transflectance at 580 nm; Transflectance at 581 nm; Transflectance at 582 nm; Transflectance at 583 nm; Transflectance at 584 nm; Transflectance at 585 nm; Transflectance at 586 nm; Transflectance at 587 nm; Transflectance at 588 nm; Transflectance at 589 nm; Transflectance at 590 nm; Transflectance at 591 nm; Transflectance at 592 nm; Transflectance at 593 nm; Transflectance at 594 nm; Transflectance at 595 nm; Transflectance at 596 nm; Transflectance at 597 nm; Transflectance at 598 nm; Transflectance at 599 nm; Transflectance at 600 nm; Transflectance at 601 nm; Transflectance at 602 nm; Transflectance at 603 nm; Transflectance at 604 nm; Transflectance at 605 nm; Transflectance at 606 nm; Transflectance at 607 nm; Transflectance at 608 nm; Transflectance at 609 nm; Transflectance at 610 nm; Transflectance at 611 nm; Transflectance at 612 nm; Transflectance at 613 nm; Transflectance at 614 nm; Transflectance at 615

Type: Dataset

Format: text/tab-separated-values, 436643 data points

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Processed Sub Bottom Profiler (SBP) data around Tristan da Cunha (2019)

Wintersteller, Paul ; Strack, Anne ; Geissler, Wolfram H

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Publication Date: 2023-03-16

Description: Sub bottom profiler (SBP) aka sediment echosounder data. Sediment echosounder measurements were conducted continuously by means of Teledyne PARASOUND DS3 (P70) parametric sediment echosounder during both R/V MARIA S. MERIAN cruises, MSM20-2 (Jegen et al., 2015) and MSM24, until the shutdown of the system due to technical reasons on cruise MSM24. The system's beam width is 4.5° along-track and 5.0° across-track. The primary high frequency signal (PHF) with a frequency of about 18 kHz was recorded for water-column investigations while the secondary low frequency signal (SLF) with a frequency of 4 kHz is used to image the shallow sub-seafloor. This selection of four PARASOUND profiles were converted into SEG-Y data by using the PS32segy tool (Hanno Keil, University of Bremen, Germany). Afterwards, the ReflexW software57 (Sandmeier, 2012) was used to low-pass filter the data and to mute the water column.

Keywords: AWI_PhyOce; Center for Marine Environmental Sciences; File format; File name; File size; GEOMAR; Helmholtz Centre for Ocean Research Kiel; MARUM; PARASOUND; Physical Oceanography @ AWI; sub bottom profiles; Tristan da Cunha; Uniform resource locator/link to file

Type: Dataset

Format: text/tab-separated-values, 20 data points

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Stable water isotope composition (δ18O and δD) of firn core FP-1 from King George Island, Antarctica (2019)

Fernandoy, Francisco ; Meyer, Hanno ; Tonelli, Marco

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Publication Date: 2023-03-16

Description: High resolution stable water isotope composition (δ18O and δD) of firn cores FP-1 retrieved at King George Island, South Shetland Islands, Antarctica. The core was sampled at 5 cm resolution at the Alfred Wegener Institute (AWI) ice core facilities in Bremerhaven, Germany. Stable water isotopes analysis were carried out at AWI in Potsdam, Germany.

Keywords: Antarctica; Antarctic Peninsula; ANT-Land_2010_AntarcticPeninsula; API2010; AWI_Envi; AWI Antarctic Land Expedition; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; FIRN; Firn auger; FP-1; ice cores; King George Island, Antarctica; Polar Terrestrial Environmental Systems @ AWI; stable water isotopes; δ18O, water; δ Deuterium, water

Type: Dataset

Format: text/tab-separated-values, 1232 data points

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Stable water isotope composition (δ18O and δD) of firn core FP-3 from King George Island, Antarctica (2019)

Fernandoy, Francisco ; Meyer, Hanno ; Tonelli, Marco

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Publication Date: 2023-03-16

Description: High resolution stable water isotope composition (δ18O and δD)of firn core FP-3 retrieved at King George Island, South Shetland Islands, Antarctica. The core was sampled at 5 cm resolution at the Alfred Wegener Institute (AWI) ice core facilities in Bremerhaven, Germany. Stable water isotopes analysis were carried out at AWI in Potsdam, Germany.

Keywords: Antarctica; Antarctic Peninsula; ANT-Land_2010_AntarcticPeninsula; API2010; AWI_Envi; AWI Antarctic Land Expedition; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; FIRN; Firn auger; FP-3; ice cores; King George Island, Antarctica; Polar Terrestrial Environmental Systems @ AWI; stable water isotopes; δ18O, water; δ Deuterium, water

Type: Dataset

Format: text/tab-separated-values, 1192 data points

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Stable water isotope composition (δ18O and δD) of firn core FP-4 from King George Island, Antarctica (2019)

Fernandoy, Francisco ; Meyer, Hanno ; Tonelli, Marco

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Publication Date: 2023-03-16

Description: High resolution stable water isotope composition (δ18O and δD) of firn core FP-4 retrieved at King George Island, South Shetland Islands, Antarctica. The core was sampled at 5 cm resolution at the Alfred Wegener Institute (AWI) ice core facilities in Bremerhaven, Germany. Stable water isotopes analysis were carried out at AWI in Potsdam, Germany.

Keywords: Antarctica; Antarctic Peninsula; ANT-Land_2010_AntarcticPeninsula; API2010; AWI_Envi; AWI Antarctic Land Expedition; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; FIRN; Firn auger; FP-4; ice cores; King George Island, Antarctica; Polar Terrestrial Environmental Systems @ AWI; stable water isotopes; δ18O, water; δ Deuterium, water

Type: Dataset

Format: text/tab-separated-values, 108 data points

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Strontium, neodymium and lead isotopes in dust from source area in northern South Australia and the northwestern corner of Western Australia, samples A, B and C (2019)

De Deckker, Patrick

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Publication Date: 2023-03-22

Keywords: DUST; Dust_A; Dust_B; Dust_C; Dust sample; Event label; Geochemical fingerprinting; Latitude of event; Lead-206/Lead-204 ratio; Lead-207/Lead-204 ratio; Lead-208; Lead-208/Lead-204 ratio; Longitude of event; Nd isotopes; Neodymium-143/Neodymium-144 ratio; Particle source area; Particle source area. Sr Nd Pb isotopes; Pb isotopes; Sample material; Site; Site A; Site B; Site C; Sr isotopes; Strontium-87/Strontium-86 ratio; Thorium; Uranium; ε-Neodymium (0)

Type: Dataset

Format: text/tab-separated-values, 30 data points

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Raw bottom track error velocity and range data from moored upward-looking Acoustic Doppler Current Profilers in the Laptev Sea between 2013 and 2015 (2019)

Belter, Hans Jakob ; Janout, Markus A ; Krumpen, Thomas ; [et al.]

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Publication Date: 2023-03-16

Description: Within the framework of the Russian-German BMBF-funded TRANSDRIFT project moored upward-looking Acoustic Doppler Current Profilers (ADCPs) were deployed in the Laptev Sea between 2013 and 2015. Two upward-looking Workhorse 300 kHz Sentinel ADCPs (manufactured by Teledyne RDI) were deployed at the 1893 and Taymyr stations in September 2013. During a Russian expedition in September 2014 both moorings were recovered and partly redeployed at the two stations until September 2015 (one upward-looking ADCP was substituted in 2014). The four data sets (ADCP_BT_1893_1314.txt, ADCP_BT_Taymyr_1314.txt, ADCP_BT_1893_1415.txt and ADCP_BT_Taymyr_1415.txt) are named to indicate the location of the deployment (station name) and the sampling period. Each file contains hourly values of error velocity (in mm/s) and range (beams 1 to 4, in m) data that was recorded using the ADCPs bottom track (BT) mode. Additionally, the instruments roll and pitch values (in deg) are included. The deployment sheets are attached as well. All moorings were equipped with numerous other instruments. Their data has been published separately.

Keywords: 1893-T1-13-ADCP; 1893-T1-14-ADCP; Acoustic Doppler Current Profiler; ADCP; ADCP_BT_1893_1314; ADCP_BT_1893_1415; ADCP_BT_Taymyr_1314; ADCP_BT_Taymyr_1415; AWI_SeaIce; bottom track; Date/Time of event; Date/Time of event 2; Event label; File content; File format; File name; File size; Laptev Sea; Laptev Sea System; Latitude of event; Longitude of event; LSS; Sea Ice Physics @ AWI; Taymyr-T1-13-ADCP; Taymyr-T1-14-ADCP; Transdrift-XXI; Transdrift-XXII; Uniform resource locator/link to file; Uniform resource locator/link to metadata file; VB13; VB14; Viktor Buynitskiy

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Format: text/tab-separated-values, 24 data points

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Biochemical investigation of multicorer sediment profile PS93/048-11 (2019)

Schewe, Ingo

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/048-11; PS93.2; S3; TVMUC

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Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/050-19 (2019)

Schewe, Ingo

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-IV; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/050-19; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/054-2 (2019)

Schewe, Ingo

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-VII; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/054-2; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/055-2 (2019)

Schewe, Ingo

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-VIII; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/055-2; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/051-4 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-V; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/051-4; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/053-3 (2019)

Schewe, Ingo

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-VI; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/053-3; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/056-1 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-IX; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/056-1; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/058-12 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; EG_IV; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/058-12; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/074-3 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/074-3; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 30 data points

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Biochemical investigation of multicorer sediment profile PS93/060-10 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; N5; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/060-10; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/066-2 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/066-2; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/077-2 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/077-2; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/078-2 (2019)

Schewe, Ingo

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In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/078-2; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Biochemical investigation of multicorer sediment profile PS93/085-2 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; N3; North Greenland Sea; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/085-2; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 25 data points

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Biochemical investigation of multicorer sediment profile PS93/080-9 (2019)

Schewe, Ingo

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

Keywords: ARK-XXIX/2.2; Carbon, organic, total; Chlorophyll a; DEPTH, sediment/rock; Esterase activity per sediment volume; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Multicorer with television; North Greenland Sea; Phaeopigments; Phospholipids; Polarstern; Porosity; Proteins, readily soluble per sediment volume; PS93/080-9; PS93.2; TVMUC

Type: Dataset

Format: text/tab-separated-values, 35 data points

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Sensitivity of tetrodotoxin and saxitoxin to changing ocean conditions (2019)

Roggatz, Christina C ; Fletcher, Nichola ; Benoit, David M ; [et al.]

PANGAEA

In: Supplement to: Roggatz, Christina C; Fletcher, Nichola; Benoit, David M; Algar, Adam C; Doroff, Angela; Wright, Bruce; Wollenberg Valero, Katharina C; Hardege, Jörg D (2019): Saxitoxin and tetrodotoxin bioavailability increases in future oceans. Nature Climate Change, https://doi.org/10.1038/s41558-019-0589-3

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Publication Date: 2023-03-16

Description: This dataset, consisting of 3 separate files, provides the basis for our manuscript entitled "Saxitoxin and tetrodotoxin bioavailability increases in future oceans". Each file contains the data for one figure. For detailed calculation methods please refer to the method and supplementary information sections of the associated manuscript. Fig1_STX_and_TTX_pH-availability contains abundance data of saxitoxin (STX) and tetrodotoxin (TTX) protonation states across the pH range from 6 to 10 at 3 different temperatures. It is calculated based on published pKa data using the Henderson-Hasselbalch equation. Temperature is taken into account employing a pKa-influencing factor of -0.2/+10C. Fig2_Dinos_HAEDAT_STX_concatenated contains all the information required for plotting the pH and temperature dependent global toxicity map. It combines georeferenced records for localities with STX-related HABs (extracted from the Harmful Algal Information System metadatabase - HAEDAT) and the distribution of two dinoflagellate genera, which are known to produce STX, Gymnodinium and Alexandrium (extracted from the NOAA COPEPOD database). For each location we also extracted current and future pH and sea surface temperature from the Global marine environment dataset (GMED)/ IPCC (WCRP CMIP3) multi-model database. We calculated the abundance of the toxic STX form based on the pH and temperature for each of the respective locations in current and future conditions. Fig3_STXinClamTissue contains the compiled total STX content in clam tissue data from the PSP Program website of the Quagan Tayagungin Tribe for the time frame between June 2012 and July 2018 for each month at Spit Beach, Sand Point (Alaska). Based on this data we further calculated the current and future toxic proportion of this total STX content for the location's specific current and future temperature and pH data.

Keywords: climate change effect; File format; File name; File size; geospatial toxicity maps; neurotoxins; Ocean acidification; pH-dependent toxicity; Uniform resource locator/link to file

Type: Dataset

Format: text/tab-separated-values, 12 data points

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Physical oceanography and current meter data from mooring F2-18 (2019)

von Appen, Wilken-Jon ; Kritsotalakis, Stylianos ; Kanzow, Torsten

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXX/2, GN05; AWI_PhyOce; CTD; Current direction; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; F2-18; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS100; PS100/016-1, MSM76_203-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 5726661 data points

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Physical oceanography and current meter data from mooring F3-17 (2019)

von Appen, Wilken-Jon ; Kritsotalakis, Stylianos ; Kanzow, Torsten

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXX/2, GN05; AWI_PhyOce; CTD; Current direction; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; F3-17; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS100; PS100/017-1, MSM76_202-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 5583742 data points

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Physical oceanography and current meter data from mooring F4-17 (2019)

von Appen, Wilken-Jon ; Schaffer, Janin ; Kanzow, Torsten

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXX/2, GN05; AWI_PhyOce; CTD; Current direction; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; F4-17; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS100; PS100/018-1, PS114_11-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 6256207 data points

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Physical oceanography and current meter data from mooring F4-S-2 (2019)

von Appen, Wilken-Jon ; Lochthofen, Normen ; Nöthig, Eva-Maria ; [et al.]

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; DATE/TIME; DEPTH, water; F4-S-2; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS107; PS107_49-1, PS114_10-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 142872 data points

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Physical oceanography and current meter data from mooring HG-EGC-4 at Hausgarten East Greenland Current (2019)

von Appen, Wilken-Jon ; Lochthofen, Normen ; Nöthig, Eva-Maria ; [et al.]

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; Current direction; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; HG-EGC-4; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS107; PS107_23-1, PS114_43-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 166370 data points

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Physical oceanography and current meter data from mooring F5-17 (2019)

von Appen, Wilken-Jon ; Kritsotalakis, Stylianos ; Kanzow, Torsten

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXX/2, GN05; AWI_PhyOce; CTD; Current direction; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; F5-17; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS100; PS100/019-1, MSM76_198-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 5728359 data points

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Physical oceanography and current meter data from mooring HG-IV-SWIPS-2017 at Hausgarten IV (2019)

von Appen, Wilken-Jon ; Lochthofen, Normen ; Nöthig, Eva-Maria ; [et al.]

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; Current direction; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; HG-IV-SWIPS-2017; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS107; PS107_38-4, PS114_3-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 91963 data points

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Physical oceanography and current meter data from mooring HG-IV-S-2 at Hausgarten IV (2019)

von Appen, Wilken-Jon ; Lochthofen, Normen ; Nöthig, Eva-Maria ; [et al.]

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; DATE/TIME; DEPTH, water; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; HG-IV-S-2; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS107; PS107_38-2, PS114_1-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 151797 data points

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Physical oceanography and current meter data from mooring HG-N-FEVI-35 at Hausgarten North (2019)

von Appen, Wilken-Jon ; Lochthofen, Normen ; Nöthig, Eva-Maria ; [et al.]

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; Current direction; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; HG-N-FEVI-35; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS107; PS107_35-1, PS114_32-1; Salinity; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 137033 data points

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Physical oceanography and current meter data from mooring Lander-2017 at Hausgarten IV (2019)

Wenzhöfer, Frank ; Soltwedel, Thomas ; Schewe, Ingo ; [et al.]

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; Current direction; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; FRAM; FRontiers in Arctic marine Monitoring; Gear identification number; Hausgarten; Lander-2017; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Oxygen; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS107; PS107_38-7, MSM77_4-9; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 28736 data points

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Raw data including physical oceanography from mooring F2-18 recovered during Maria S. Merian cruise MSM76 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXX/2, GN05; AWI_PhyOce; CTD; F2-18; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS100; PS100/016-1, MSM76_203-1

Type: Dataset

Format: application/zip, 1.4 GBytes

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Raw data including physical oceanography from mooring F3-17 recovered during Maria S. Merian cruise MSM76 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXX/2, GN05; AWI_PhyOce; CTD; F3-17; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS100; PS100/017-1, MSM76_202-1

Type: Dataset

Format: application/zip, 1.6 GBytes

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Raw data including physical oceanography from mooring F4-17 recovered during during POLARSTERN cruise PS114 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXX/2, GN05; AWI_PhyOce; CTD; F4-17; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS100; PS100/018-1, PS114_11-1

Type: Dataset

Format: application/zip, 1.4 GBytes

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Raw data including physical oceanography from mooring F4-S-2 recovered during POLARSTERN cruise PS114 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; F4-S-2; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS107; PS107_49-1, PS114_10-1

Type: Dataset

Format: application/zip, 3.2 MBytes

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Raw data including physical oceanography from mooring F5-17 recovered during Maria S. Merian cruise MSM76 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXX/2, GN05; AWI_PhyOce; CTD; F5-17; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS100; PS100/019-1, MSM76_198-1

Type: Dataset

Format: application/zip, 1.4 GBytes

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Raw data including physical oceanography from mooring HG-EGC-4 recovered during POLARSTERN cruise PS114 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-EGC-4; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS107; PS107_23-1, PS114_43-1

Type: Dataset

Format: application/zip, 1.1 MBytes

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Raw data including physical oceanography from mooring HG-IV-S-2 recovered during POLARSTERN cruise PS114 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-IV-S-2; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS107; PS107_38-2, PS114_1-1

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Format: application/zip, 5.2 MBytes

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Raw data including physical oceanography from mooring HG-IV-SWIPS-2017 recovered during POLARSTERN cruise PS107 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-IV-SWIPS-2017; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS107; PS107_38-4, PS114_3-1

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Format: application/zip, 14.5 MBytes

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Raw data including physical oceanography from mooring HG-N-FEVI-35 recovered during POLARSTERN cruise PS114 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; HG-N-FEVI-35; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS107; PS107_35-1, PS114_32-1

Type: Dataset

Format: application/zip, 1.1 MBytes

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Raw data including physical oceanography from mooring Lander-2017 recovered during Maria S. Merian cruise MSM77 (2019)

von Appen, Wilken-Jon

PANGAEA

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Publication Date: 2023-03-16

Keywords: ADCP; ARK-XXXI/2; AWI_PhyOce; CTD; FRAM; FRontiers in Arctic marine Monitoring; Hausgarten; Lander-2017; Long-term Investigation at AWI-Hausgarten off Svalbard; Mooring; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS107; PS107_38-7, MSM77_4-9

Type: Dataset

Format: application/zip, 502.2 kBytes

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Sea ice drift and surface temperature from autonomous measurements from buoy 2017C22, deployed during TIFAX 2017 (2019)

Krumpen, Thomas ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: Sea ice drift and surface temperature were measured by the Compact Air-Launched Ice Beacon (CALIB) 2017C22 drifting on Arctic multi year sea ice deployed by air-plane drop off during TIFAX 2017. The time series describes the position and additional parameters of the buoy between 19 Aug 2017 and 23 July 2018 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).

Keywords: 2017C22; Arctic Ocean; autonomous platform; AWI_SeaIce; buoy; Buoy, Compact Air-Launched Ice Beacon; CALIB; DATE/TIME; drift; LATITUDE; LONGITUDE; Sea ice; Sea Ice Physics @ AWI; snow depth; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 8121 data points

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Sea ice drift, surface temperature, and barometric pressure from autonomous measurements from buoy 2018C27, deployed during ASIMBO 2018 (2019)

Haas, Christian ; Goessling, Helge ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: Sea ice drift, surface temperature, and barometric pressure were measured by the Compact Air-Launched Ice Beacon (CALIB) 2018C27 drifting on Arctic sea ice deployed by air-plane drop off during ASIMBO 2018. The time series describes the position and additional parameters of the buoy between 13 August 2018 and 30 January 2019 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).

Keywords: 2018C27; Arctic Ocean; autonomous platform; AWI_SeaIce; buoy; Buoy, Compact Air-Launched Ice Beacon; CALIB; DATE/TIME; drift; LATITUDE; LONGITUDE; Pressure, atmospheric; Sea Ice Physics @ AWI; snow depth; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 8172 data points

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Sea ice drift and surface temperature from autonomous measurements from buoy 2019C30, deployed during IceBird 2019 Winter (2019)

Hendricks, Stefan ; Ricker, Robert

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: Sea ice drift and surface temperature were measured by the Compact Air-Launched Ice Beacon (CALIB) 2019C30 drifting on Arctic sea ice deployed via aircraft gravity launcher during IceBird 2019 Winter. The time series describes the position and additional parameters of the buoy between 05 April 2019 and 28 June 2019 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).

Keywords: 2019C30; Arctic Ocean; autonomous platform; AWI_SeaIce; buoy; Buoy, Compact Air-Launched Ice Beacon; CALIB; DATE/TIME; drift; LATITUDE; LONGITUDE; Sea Ice Physics @ AWI; snow depth; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 2014 data points

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Sea ice drift and surface temperature from autonomous measurements from buoy 2019C31, deployed during IceBird 2019 Winter (2019)

Hendricks, Stefan ; Ricker, Robert

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: Sea ice drift and surface temperature were measured by the Compact Air-Launched Ice Beacon (CALIB) 2019C31 drifting on Arctic sea ice deployed via aircraft gravity launcher during IceBird 2019 Winter. The time series describes the position and additional parameters of the buoy between 05 April 2019 and 10 July 2019 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).

Keywords: 2019C31; Arctic Ocean; autonomous platform; AWI_SeaIce; buoy; Buoy, Compact Air-Launched Ice Beacon; CALIB; DATE/TIME; drift; LATITUDE; LONGITUDE; Sea Ice Physics @ AWI; snow depth; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 2287 data points

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Sea ice drift and surface temperature from autonomous measurements from buoy 2019C32, deployed during IceBird 2019 Winter (2019)

Haas, Christian ; Nicolaus, Marcel

PANGAEA

In: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven

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Publication Date: 2023-03-16

Description: Sea ice drift, surface temperature, and barometric pressure were measured by the Compact Air-Launched Ice Beacon (CALIB) 2017C32 drifting on Arctic first year sea ice deployed during a landing by Twin Otter for the CryoVEx 2017 project. The time series describes the position and additional parameters of the buoy between 18 April 2017 and 11 February 2018 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).

Keywords: 2017C32; autonomous platform; AWI_SeaIce; buoy; Buoy, Compact Air-Launched Ice Beacon; CALIB; DATE/TIME; drift; LATITUDE; Lincoln Sea; LONGITUDE; Pressure, atmospheric; Sea Ice Physics @ AWI; snow depth; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 14374 data points

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Stable isotope characteristics of precipitation in southeast Siberia (2019)

Kostrova, Svetlana S ; Meyer, Hanno ; Fernandoy, Francisco ; [et al.]

PANGAEA

In: Supplement to: Kostrova, Svetlana S; Meyer, Hanno; Fernandoy, Francisco; Werner, Martin; Tarasov, Pavel E (2020): Moisture origin and stable isotope characteristics of precipitation in southeast Siberia. Hydrological Processes, 34(1), 51-67, https://doi.org/10.1002/hyp.13571

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Publication Date: 2023-03-16

Description: The paper presents oxygen and hydrogen isotopes of 284 precipitation event samples systematically collected in Irkutsk, in the Baikal region (southeast Siberia), between June 2011 and April 2017. This is the first high-resolution dataset of stable isotopes of precipitation from this poorly studied region of continental Asia, which has a high potential for isotope-based palaeoclimate research. The dataset revealed distinct seasonal variations: relatively high δ¹⁸O (up to -4‰) and δD (up to -40‰) values characterize summer air masses, and lighter isotope composition (-41‰ for δ¹⁸O and -322‰ for δD) is characteristic of winter precipitation. Our results show that air temperature mainly affects the isotope composition of precipitation, and no significant correlations were obtained for precipitation amount and relative humidity. A new temperature dependence was established for weighted mean monthly precipitation: +0.50‰/°C (r² = 0.83; p 〈 0.01; n = 55) for δ¹⁸O and +3.8‰/°C (r² = 0.83, p 〈 0.01; n = 55) for δD. Secondary fractionation processes (e.g., contribution of recycled moisture) were identified mainly in summer from low d excess. Backward trajectories assessed with the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) model indicate that precipitation with the lowest mean δ¹⁸O and δD values reaches Irkutsk in winter related to moisture transport from the Arctic. Precipitation originating from the west/southwest with the heaviest mean isotope composition reaches Irkutsk in summer, thus representing moisture transport across Eurasia. Generally, moisture transport from the west, that is, the Atlantic Ocean predominates throughout the year. A comparison of our new isotope dataset with simulation results using the European Centre/Hamburg version 5 (ECHAM5)-wiso climate model reveals a good agreement of variations in δ¹⁸O (r² = 0.87; p 〈 0.01; n = 55) and air temperature (r² = 0.99; p 〈 0.01; n = 71). However, the ECHAM5-wiso model fails to capture observed variations in d excess (r² = 0.14; p 〈 0.01; n = 55). This disagreement can be partly explained by a model deficit of capturing regional hydrological processes associated with secondary moisture supply in summer.

Keywords: AWI_Envi; DATE/TIME; Deuterium excess; Irkutsk_prec; Irkutsk, Russia; Polar Terrestrial Environmental Systems @ AWI; Sample code/label; Sample type; Water sample; WS; δ18O, water; δ Deuterium, water

Type: Dataset

Format: text/tab-separated-values, 1420 data points

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Glyoxal- and formaldehyde slant column densities measured during the cruise MSM58/2 over the Atlantic Ocean using MAX-DOAS (2019)

Behrens, Lisa K ; Hilboll, Andreas ; Richter, Andreas ; [et al.]

PANGAEA

In: Supplement to: Behrens, Lisa K; Hilboll, Andreas; Richter, Andreas; Peters, Enno; Alvarado, Leonardo M A; Kalisz Hedegaard, Anna Beata; Wittrock, Folkard; Burrows, John Philipp; Vrekoussis, Mihalis (2019): Detection of outflow of formaldehyde and glyoxal from the African continent to the Atlantic Ocean with a MAX-DOAS instrument. Atmospheric Chemistry and Physics, 19(15), 10257-10278, https://doi.org/10.5194/acp-19-10257-2019

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Publication Date: 2023-03-07

Description: Trace gas maps retrieved from satellite measurements show enhanced levels of the atmospheric volatile organic compounds formaldehyde (HCHO) and glyoxal (CHOCHO) over the Atlantic Ocean. To validate the spatial distribution of this continental outflow, ship-based measurements were taken during the Continental Outflow of Pollutants towards the MArine tRoposphere (COPMAR) project. A Multi-AXis Differential Optical Absorption Spectrometer (MAX-DOAS) was operated aboard the research vessel (RV) Maria S. Merian during cruise MSM58/2. This cruise was conducted in October 2016 from Ponta Delgada (Azores) to Cape Town (South Africa), crossing between Cabo Verde and the African continent. The instrument was continuously scanning the horizon, looking towards the African continent. Enhanced levels of HCHO and CHOCHO were found in the area of expected outflow during this cruise. The observed spatial gradients of HCHO and CHOCHO along the cruise track agree with the spatial distributions from satellite measurements and the Model for OZone and Related chemical Tracers version 4 (MOZART-4) model simulations. The continental outflow from the African continent is observed in an elevated layer, higher than 1000 m, and probably originates from biogenic emissions or biomass burning according to FLEXible PARTicle dispersion model (FLEXPART) emission sensitivities.

Type: Dataset

Format: application/zip, 2 datasets

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170

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Sky photos from the agricultural Gebesee test site (central Germany) in 2016 (2019)

Truckenbrodt, Sina C

PANGAEA

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Publication Date: 2023-03-07

Keywords: Agriculture; Application of the EO-LDAS Prototype and Data Base to Prepare Sentinel-2 Assimilation; Atmosphere; Biochemical parameter; Biophysical parameter; Biosphere; Cereals; Crop; Earth observation; EO-LDAS; EO-LDAS-App; File format; File name; File size; Gebesee test site; Hyperspectral data; In situ; Potato; remote sensing; Soil; Spring wheat; Sugar beet; Uniform resource locator/link to file; Winter barley; Winter wheat

Type: Dataset

Format: text/tab-separated-values, 20 data points

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Phenology photos from the agricultural Gebesee test site (central Germany) in 2016 (2019)

Truckenbrodt, Sina C

PANGAEA

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Publication Date: 2023-03-07

Keywords: Agriculture; Application of the EO-LDAS Prototype and Data Base to Prepare Sentinel-2 Assimilation; Atmosphere; Biochemical parameter; Biophysical parameter; Biosphere; Cereals; Crop; Earth observation; EO-LDAS; EO-LDAS-App; File format; File name; File size; Gebesee test site; Hyperspectral data; In situ; Potato; remote sensing; Soil; Spring wheat; Sugar beet; Uniform resource locator/link to file; Winter barley; Winter wheat

Type: Dataset

Format: text/tab-separated-values, 20 data points

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Mean and standard deviation of hyperspectral surface reflectance acquired on the agricultural Gebesee test site (central Germany) in 2016 (2019)

Truckenbrodt, Sina C

PANGAEA

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Publication Date: 2023-03-07

Keywords: Agriculture; Application of the EO-LDAS Prototype and Data Base to Prepare Sentinel-2 Assimilation; Atmosphere; Biochemical parameter; Biophysical parameter; Biosphere; Cereals; Crop; Earth observation; EO-LDAS; EO-LDAS-App; Gebesee test site; Hyperspectral data; In situ; Potato; remote sensing; Soil; Spring wheat; Sugar beet; Winter barley; Winter wheat

Type: Dataset

Format: application/zip, 586 kBytes

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Agricultural Gebesee test site (central Germany): extent and location of acreages investigated in 2016 (2019)

Truckenbrodt, Sina C

PANGAEA

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Publication Date: 2023-03-07

Keywords: Agriculture; Application of the EO-LDAS Prototype and Data Base to Prepare Sentinel-2 Assimilation; Atmosphere; Biochemical parameter; Biophysical parameter; Biosphere; Cereals; Crop; Earth observation; EO-LDAS; EO-LDAS-App; Gebesee test site; Hyperspectral data; In situ; Potato; remote sensing; Soil; Spring wheat; Sugar beet; Winter barley; Winter wheat

Type: Dataset

Format: application/zip, 3.1 kBytes

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174

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Photos of the landscape of the agricultural Gebesee test site (central Germany) in 2016 (2019)

Truckenbrodt, Sina C

PANGAEA

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Publication Date: 2023-03-07

Keywords: Agriculture; Application of the EO-LDAS Prototype and Data Base to Prepare Sentinel-2 Assimilation; Atmosphere; Biochemical parameter; Biophysical parameter; Biosphere; Cereals; Crop; Earth observation; EO-LDAS; EO-LDAS-App; File format; File name; File size; Gebesee test site; Hyperspectral data; In situ; Potato; remote sensing; Soil; Spring wheat; Sugar beet; Uniform resource locator/link to file; Winter barley; Winter wheat

Type: Dataset

Format: text/tab-separated-values, 20 data points

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Morphological and genetic data from Cnemidocarpa verrucosa sensu lato (2019)

Ruiz, Micaela Belen ; Taverna, Anabela ; Sahade, Ricardo José ; [et al.]

PANGAEA

In: Supplement to: Ruiz, Micaela Belen; Taverna, Anabela; Servetto, Natalia; Sahade, Ricardo José; Held, Christoph (2020): Hidden diversity in Antarctica: Molecular and morphological evidence of two different species within one of the most conspicuous ascidian species. Ecology and Evolution, https://doi.org/10.1002/ece3.6504

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Publication Date: 2023-03-07

Description: The Southern Ocean is one of the most isolated marine ecosystems, characterized by high levels of endemism, diversity and biomass. Ascidians are among the dominant groups in the Antarctic benthic communities, thus recording the evolutionary patterns of this group is crucial to improve our current understanding on the assembly of this polar ocean. In this study, we studied the genetic variation within Cnemidocarpa verrucosa sensu lato, one of the most widely distributed and abundant ascidians in Antarctica. Using a mitochondrial and a nuclear gene (mtCOI and 18S), the phylogeography of fifteen populations distributed along the Antarctic Peninsula and South America (Burdwood Bank/MPA Namuncurá) was characterized, where the bimodal distribution of the genetic distance suggested the existence of two species within the nominal C. verrucosa. When re-evaluating morphological traits to distinguish between genetically defined species, the presence of basal disc in one of the genotypes allowed to differentiate the species.

Keywords: Branchial formula; Carlini_Base; Cnemidocarpa verrucosa, height; Cnemidocarpa verrucosa, number of gonads; Cnemidocarpa verrucosa, number of stomach folds; Cnemidocarpa verrucosa, width; Color description; DEPTH, water; Number; Potter Peninsula, King George Island, Western Antarctica; Presence/absence; Research station; RS; Sample ID; Shape; Siphon, position; Species, genetic

Type: Dataset

Format: text/tab-separated-values, 288 data points

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Protactinium, thorium, uranium and opal of sediment core KNR140-12JPC (2019)

Süfke, Finn

PANGAEA

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Publication Date: 2023-03-10

Keywords: AGE; Blake Ridge; Comment; Core; DEPTH, sediment/rock; Knorr; KNR140; KNR140-12JPC; KNR140-2-12JPC; Opal, biogenic silica; Opal, biogenic silica, error, relative; Pa/Th; PC; Piston corer; Protactinium; Protactinium-231; Protactinium-231, error, relative; Protactinium-231/Thorium-230, error, relative; Protactinium-231/Thorium-230 ratio; South Atlantic Ocean; Thorium; Thorium-230; Thorium-230, error, relative; Thorium-232; Thorium-232, error, relative; Uranium-238; Uranium-238, error, relative

Type: Dataset

Format: text/tab-separated-values, 234 data points

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Physical oceanography during Celtic Explorer cruise 2005 (2019)

Müller, Gerd

PANGAEA

In: Institut für Meereskunde, Universität Hamburg

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Publication Date: 2023-03-10

Description: Müller, Gerd (2005): Hydrographic observations in the Norwegian Sea from 23. February - 17. March 2005 during the Celtic Explorer cruise 2005

Keywords: 1; 10; 100; 101; 102; 103; 104; 105; 106; 107; 108; 109; 11; 110; 111; 112; 113; 114; 115; 116; 117; 118; 119; 12; 120; 121; 122; 123; 124; 125; 126; 127; 128; 129; 13; 130; 131; 132; 133; 134; 14; 15; 16; 17; 18; 19; 2; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 3; 30; 31; 32; 33; 34; 35; 36; 38; 39; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 50; 51; 52; 53; 54; 55; 56; 57; 58; 59; 6; 60; 61; 62; 63; 64; 65; 66; 67; 68; 69; 7; 70; 71; 72; 73; 74; 75; 76; 77; 78; 79; 8; 80; 81; 82; 83; 84; 85; 86; 87; 88; 89; 9; 90; 91; 92; 93; 94; 95; 96; 97; 98; 99; CE050X; CE050X_001; CE050X_002; CE050X_003; CE050X_006; CE050X_007; CE050X_008; CE050X_009; CE050X_010; CE050X_011; CE050X_012; CE050X_013; CE050X_014; CE050X_015; CE050X_016; CE050X_017; CE050X_018; CE050X_019; CE050X_020; CE050X_021; CE050X_022; CE050X_023; CE050X_024; CE050X_025; CE050X_026; CE050X_027; CE050X_028; CE050X_029; CE050X_030; CE050X_031; CE050X_032; CE050X_033; CE050X_034; CE050X_035; CE050X_036; CE050X_038; CE050X_039; CE050X_040; CE050X_041; CE050X_042; CE050X_043; CE050X_044; CE050X_045; CE050X_046; CE050X_047; CE050X_048; CE050X_049; CE050X_050; CE050X_051; CE050X_052; CE050X_053; CE050X_054; CE050X_055; CE050X_056; CE050X_057; CE050X_058; CE050X_059; CE050X_060; CE050X_061; CE050X_062; CE050X_063; CE050X_064; CE050X_065; CE050X_066; CE050X_067; CE050X_068; CE050X_069; CE050X_070; CE050X_071; CE050X_072; CE050X_073; CE050X_074; CE050X_075; CE050X_076; CE050X_077; CE050X_078; CE050X_079; CE050X_080; CE050X_081; CE050X_082; CE050X_083; CE050X_084; CE050X_085; CE050X_086; CE050X_087; CE050X_088; CE050X_089; CE050X_090; CE050X_091; CE050X_092; CE050X_093; CE050X_094; CE050X_095; CE050X_096; CE050X_097; CE050X_098; CE050X_099; CE050X_100; CE050X_101; CE050X_102; CE050X_103; CE050X_104; CE050X_105; CE050X_106; CE050X_107; CE050X_108; CE050X_109; CE050X_110; CE050X_111; CE050X_112; CE050X_113; CE050X_114; CE050X_115; CE050X_116; CE050X_117; CE050X_118; CE050X_119; CE050X_120; CE050X_121; CE050X_122; CE050X_123; CE050X_124; CE050X_125; CE050X_126; CE050X_127; CE050X_128; CE050X_129; CE050X_130; CE050X_131; CE050X_132; CE050X_133; CE050X_134; Celtic Explorer; Conductivity; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; Latitude of event; Longitude of event; Norwegian Sea; Pressure, water; Salinity; South Atlantic Ocean; Temperature, water; UniHH_CTD

Type: Dataset

Format: text/tab-separated-values, 570600 data points

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Hydrothermal cleft monazite SIMS Th-Pb age data, central Alps (2019)

Bergemann, Christian A ; Gnos, Edwin ; Berger, Alfons ; [et al.]

PANGAEA

In: Supplement to: Bergemann, Christian A; Gnos, Edwin; Berger, Alfons; Janots, Emilie; Whitehouse, Martin J (2020): Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce). Solid Earth, 11(1), 199-222, https://doi.org/10.5194/se-11-199-2020

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Publication Date: 2023-02-25

Description: Ion probe (SIMS) Th-Pb age measurements of hydrothermal fissure/cleft monazite from the central Alps. The sample area encompasses most of the Lepontine metamorphic dome, the eastern Rhone-Simplon Line, southern Gotthard Nappe and the Forcola Fault. The ages directly date deformation during part of the exhumation and cooling history of the Lepontine dome and deformation along the Rhone-Simplon fault zone. The ages of all crystals range from ca. 19 to 5 Ma, with age distribution and internal crystal structure facilitating to distinguish between areas whose deformational history was dominated by distinct tectonic events or continuous exhumation.

Keywords: Age, error; Age, Lead-Thorium; Age, mineral; Alpe Devero, Val Antigorio; BETT11; Bettelbach, Niederwald, Goms; BLAS1; Cava Maddalena, Beura; Crino Baceno; Doru, Gantertal, Simplon; DURO1; DURO2; DUTH2; DUTH3; DUTH6; Error, absolute; Error, relative; Event label; GRAESER1; GRAESER3; Griessgletscher; Grosses Arsch, Blinnental; KLEM1; KLEM2; KLEM3; Laercheltini, Binntal; Lago Retica, Lagi di Campo Blenio; Lago Sucro, Val Cadlimo; Lead; Lead-204/Lead-208, error, relative; Lead-204/Lead-208 ratio; Lead-208/Thorium-232, error, relative; Lead-208/Thorium-232 ratio; LUCO1; Lucomagno; Montecrstese; MULT; Multiple investigations; Original value; Parameter; Piz, Scai; Piz Blas, Val Nalps, Sedrun; Pizzo Ruescada, Valle di Prato (Lavizzara); Pizzo Tambo, Spluegen; Ratio; SALZ2; Sample code/label; Sample code/label 2; SCHIESS1; Schiessbach/Simplon; Secondary ion mass spectrometry (SIMS); TAMB1; Thorium; Thorium/Uranium ratio; Uranium; VALS; Vals, Valsertal; VANI4; VANI5; VANI6; Wannigletscher, Cherbadung, Binntal

Type: Dataset

Format: text/tab-separated-values, 8550 data points

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Carbon isotopes record in the Southeast Pacific (2019)

Martínez Fontaine, Consuelo ; De Pol-Holz, Ricardo ; Michel, Elisabeth ; [et al.]

PANGAEA

In: Supplement to: Martínez Fontaine, Consuelo; De Pol-Holz, Ricardo; Michel, Elisabeth; Siani, Giuseppe; Reyes-Macaya, Dharma; Martínez Méndez, Gema; DeVries, Tim; Stott, Lowell D; Southon, John; Mohtadi, Mahyar; Hebbeln, Dierk (2019): Ventilation of the deep ocean carbon reservoir during the last deglaciation: results from the southeast pacific. Paleoceanography and Paleoclimatology, 34(12), 2080-2097, https://doi.org/10.1029/2019PA003613

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Publication Date: 2023-03-03

Description: Supplementary material for Martínez Fontaine et al., 2019 (Table S1), including the radiocarbon ages in benthonic and planktonic foraminifera in six cores in the Chilean margin, beetween ~31°S and ~36°S (Table S3). The age models for the cores are detailed in Martínez Fontaine et al., 2019 and were produced using the information on planktonic δ13C (Table S2). Also included are the Δ14C resulting from the age models.

Keywords: Center for Marine Environmental Sciences; Deglaciation; MARUM; radiocarbon; Southeast Pacific

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Format: application/zip, 2 datasets

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Reconstructed sea surface temperature of sediment core GeoB16224-1, off French Guiana (2019)

Crivellari, Stefano ; Chiessi, Cristiano Mazur ; Kuhnert, Henning ; [et al.]

PANGAEA

In: Supplement to: Crivellari, Stefano; Chiessi, Cristiano Mazur; Kuhnert, Henning; Häggi, Christoph; Mollenhauer, Gesine; Hefter, Jens; Portilho-Ramos, Rodrigo Costa; Schefuß, Enno; Mulitza, Stefan (2019): Thermal response of the western tropical Atlantic to slowdown of the Atlantic Meridional Overturning Circulation. Earth and Planetary Science Letters, 519, 120-129, https://doi.org/10.1016/j.epsl.2019.05.006

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Publication Date: 2023-03-03

Description: The western tropical Atlantic plays an important role in the interhemispheric redistribution of heat during millennial-scale changes in the strength of the Atlantic Meridional Overturning Circulation (AMOC). The proper evaluation of this role depends on a clear understanding of sea surface temperature (SST) variations during AMOC slowdown periods like Heinrich Stadials (HS) in the western tropical Atlantic. However, published SST records from the western tropical Atlantic between ca. 4°S and 7°N show inconsistencies that are apparently related to the employed temperature proxy (i.e., Mg/Ca versus alkenone unsaturation index U37k′). In general, while Mg/Ca values indicate warming during Heinrich Stadials, U37k′ values show cooling. To assess this issue, we sampled core GeoB16224-1 retrieved off French Guiana (i.e., 6°39.38′N) and reconstructed water temperatures at high resolution using Mg/Ca on the foraminifera species Globigerinoides ruber, U37k′, TEX86 and modern analogue technique (MAT) transfer functions using planktonic foraminifera assemblages calibrated for 50 m water depth. Our results show that Mg/Ca and TEX86 values recorded an increase in SST related to AMOC slowdown. Conversely, U37k′ and MAT values registered a decrease in temperatures during HS3 and HS1. Our U37k′ and Mg/Ca results thus confirm the previously reported inconsistency for the period between 48-13 cal ka BP. We suggest that several non-thermal physiological effects probably imparted a negative temperature bias on the U37k′ temperatures during Heinrich Stadials. However, MAT-based temperatures show similar variability with U37k′-based temperatures. Hence, we also suggest that during severe slowdown periods of the AMOC, a steeper meridional temperature gradient together with a southward shift of the Intertropical Convergent Zone produced not only an increase in SST but also a stronger upper water column stratification and a shoaling of the thermocline, decreasing subsurface temperatures. Our new high resolution temperature records allow a better characterization of the thermal response of the upper water column in the tropical western Atlantic to slowdown events of the AMOC, reconciling previously discrepant records.

Keywords: Center for Marine Environmental Sciences; Heinrich Stadials; MARUM; Mg/Ca; modern analogue technique; TEX86; tropical Atlantic; UK'37

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Format: application/zip, 4 datasets

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Interaction of a deep-sea current with a blind submarine canyon (Mar del Plata Canyon, Argentina) (2019)

Warratz, Grit ; Schwenk, Tilmann ; Voigt, Ines ; [et al.]

PANGAEA

In: Supplement to: Warratz, Grit; Schwenk, Tilmann; Voigt, Ines; Bozzano, Graziella; Henrich, Rüdiger; Violante, Roberto; Lantzsch, Hendrik (2019): Interaction of a deep-sea current with a blind submarine canyon (Mar del Plata Canyon, Argentina). Marine Geology, 417, 106002, https://doi.org/10.1016/j.margeo.2019.106002

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Publication Date: 2023-03-03

Description: The Mar del Plata (MdP) Canyon at the Argentine continental margin is incorporated into a major contourite depositional system, built by the incursion of southern-sourced water masses affecting the seafloor at different waters depths. The new sedimentological, morphological and hydro acoustic data provide novel insights into contour and turbidity current interactions in mid-slope (blind) canyons, which do not have a connection to the shelf or an onshore river system. Such canyons are capable to record climate-related ocean stratification changes, current variability, and slope stability. Three sediment cores were obtained along the MdP Canyon thalweg covering the last 20,000 years and compiled with two cores from the adjacent Ewing Terrace. Turbidity-current activity within the MdP Canyon was limited to the time interval from Last Glacial Maximum (LGM) to the late deglacial. During the LGM and early deglacial, turbidites reached both the proximal sector and the distal northern flank of the canyon. During the late deglacial only the proximal sector was characterized by turbidite deposition. Similarities in mineralogy and grain-size data indicate that the material transported by the turbidity currents originated from the mid-slope Ewing Terrace. Glacial turbidity-current activity was most probably favored by increased sediment supply along the Ewing Terrace from a shallowed and/or enhanced glacial Antarctic Intermediate Water (AAIW) nepheloid layer. These sediments were trapped by the MdP Canyon, in particular at the head area. During the late deglacial, a displacement or limited AAIW nepheloid layer resulted in less sediment transfer along the Ewing Terrace and immediate accumulation in the MdP Canyon head restricting turbidite deposition to the proximal sector of the canyon. In general, contourite-turbidite interactions provide valuable information on variations in thermohaline circulation such as AAIW distribution and current strength.

Keywords: Argentina; Center for Marine Environmental Sciences; contourite; Mar del Plata Canyon; MARUM; turbidite

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Format: application/zip, 5 datasets

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GIS based analysis, processed sub bottom profiler, and composite grid and backscatter mosaics around Tristan da Cunha (2019)

Geissler, Wolfram H ; Wintersteller, Paul ; Strack, Anne ; [et al.]

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Publication Date: 2023-03-03

Description: Tristan da Cunha is assumed to be the youngest subaerial expression of the Walvis Ridge hot spot. Based on new hydroacoustic data, we propose that the most recent hot spot volcanic activity occurs west of the island. We surveyed relatively young intraplate volcanic fields and scattered, probably monogenetic, submarine volcanoes with multibeam echosounders and sub-bottom profilers. Structural and zonal GIS analysis of bathymetric and backscatter results, based on habitat mapping algorithms to discriminate seafloor features, revealed numerous previously-unknown volcanic structures. South of Tristan da Cunha, we discovered two large seamounts. One of them, Isolde Seamount, is most likely the source of a 2004 submarine eruption known from a pumice stranding event and seismological analysis. An oceanic core complex, identified at the intersection of the Tristan da Cunha Transform and Fracture Zone System with the Mid-Atlantic Ridge, might indicate reduced magma supply and, therefore, weak plume-ridge interaction at present times.

Keywords: Center for Marine Environmental Sciences; MARUM

Type: Dataset

Format: application/zip, 3 datasets

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B, Mg, Li, and Sr isotopes in acid-sulfate fluids and volcanic rocks from the Manus Basin, Papua New Guinea (2019)

Wilckens, Frederike Kristina ; Reeves, Eoghan P ; Bach, Wolfgang ; [et al.]

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Publication Date: 2023-03-03

Description: The dataset contains B, Li, Mg and Sr concentrations and isotopic compositions of black-smoker, acid-sulfate fluids and "hybrid-types" as well as of fresh and altered rocks from different vent fields (DESMOS and North Su) within the Manus Basin, Papua New Guinea. The data is used to understand the controls of their compositional variability. In particular, the formation of acid-sulfate and hybrid smoker fluids is still poorly understood, and their high Mg concentrations are explained either by dissolution of Mg-bearing minerals in the basement or by mixing between unmodified seawater and magmatic fluids. Mg isotope ratios of the acid-sulfate fluids from Manus Basin are seawater-like, which supports the idea that acid-sulfate fluids in this study area predominantly form by mixing between unmodified seawater and a Mg-free magmatic fluid. Changes in the B, Li, and Sr isotope ratios relative to seawater indicate water-rock interaction in all acid-sulfate fluids. Further, the combination of δ7Li with B concentrations of the same fluids links changes in δ7Li to changes in (1) basement alteration, (2) water-to-rock ratios during water-rock interaction and/or (3) the reaction temperature. These isotope systems, thus, allow tracing of basement composition and acid-sulfate driven alteration of the backarc crust, and help increase our understanding of hydrothermal fluid-rock interactions and the behavior of fluid-mobile elements.

Keywords: acid-sulfate; argillic alteration; back-arc; basalt; Center for Marine Environmental Sciences; hydrothermal circulation; Li isotopes; magmatic degassing; MARUM; Mg isotopes; Sr isotopes. alteration; vent fluids

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Format: application/zip, 2 datasets

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Water velocity profiles in the transect Langanes-NE from LADCP from several cruises (2019)

Semper, Stefanie ; Valdimarsson, Héðinn ; Pickart, Robert ; [et al.]

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Publication Date: 2023-03-02

Keywords: B1/2011; B1/2011_60; B1/2011_61; B1/2011_62; B1/2011_63; B1/2011_64; B1/2011_65; B1/2011_66; B1/2011_67; B1/2011_68; B1/2011_70; B1/2011_71; B1/2011_72; B1/2011_74; B1/2013; B1/2013_76; B1/2013_77; B1/2013_78; B1/2013_79; B1/2013_80; B1/2013_81; B1/2013_82; B1/2013_83; B1/2013_84; B1/2013_85; B1/2013_86; B1/2013_87; B10/2009; B10/2009_587; B10/2009_588; B10/2009_589; B10/2009_590; B10/2009_591; B10/2009_592; B10/2009_593; B10/2009_594; B10/2009_595; B10/2009_596; B10/2009_597; B10/2009_598; B10/2009_599; B10/2009_600; B10/2009_601; B10/2009_602; B11/2017; B11/2017_789; B11/2017_790; B11/2017_791; B11/2017_792; B11/2017_793; B11/2017_794; B11/2017_795; B11/2017_796; B11/2017_797; B11/2017_798; B11/2017_799; B11/2017_800; B11/2017_801; B2/2012; B2/2012_84; B2/2012_85; B2/2012_86; B2/2012_87; B2/2012_88; B2/2012_89; B2/2012_90; B2/2012_91; B2/2012_92; B2/2012_93; B2/2012_94; B2/2012_95; B7/2015; B7/2015_427; B7/2015_441; B7/2015_442; B7/2015_443; B7/2015_444; B7/2015_445; B7/2015_446; B7/2015_447; B7/2015_448; B7/2015_449; B7/2015_450; B7/2015_451; B7/2015_452; Bjarni Saemundsson; CTD/Rosette; CTD-RO; Current velocity, east-west; Current velocity, north-south; DATE/TIME; Depth, bottom/max; DEPTH, water; Event label; Håkon Mosby; HM2016618; HM2016618_876; HM2016618_877; HM2016618_878; HM2016618_879; HM2016618_880; HM2016618_881; HM2016618_882; HM2016618_883; HM2016618_884; HM2016618_885; HM2016618_886; HM2016618_887; HM2016618_888; KB2018614; KB2018614_597; KB2018614_598; KB2018614_599; KB2018614_600; KB2018614_601; KB2018614_602; KB2018614_604; KB2018614_605; KB2018614_606; KB2018614_607; KB2018614_608; KB2018614_609; KN203-2; KN203-2_175; KN203-2_176; KN203-2_177; KN203-2_178; KN203-2_179; KN203-2_180; KN203-2_181; KN203-2_182; KN203-2_183; KN203-2_184; KN203-2_185; KN203-2_186; KN203-2_187; KN203-2_188; KN203-2_189; KN203-2_190; KN203-2_191; KN203-2_192; KN203-2_193; KN203-2_194; Knorr; Kristine Bonnevie; LATITUDE; LONGITUDE; Lowered Acoustic Doppler Current Profiler (LADCP); MULT; Multiple investigations; North Atlantic

Type: Dataset

Format: text/tab-separated-values, 34590 data points

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Water velocity profiles in the transect Kolbeinsey Ridge from LADCP from several cruises (2019)

Semper, Stefanie ; Pickart, Robert ; Valdimarsson, Héðinn ; [et al.]

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Publication Date: 2023-03-02

Keywords: B7/2015; B7/2015_471; B7/2015_472; B7/2015_473; B7/2015_474; B7/2015_475; B7/2015_476; B7/2015_477; B7/2015_478; B7/2015_479; B7/2015_480; B7/2015_481; B7/2015_482; B7/2015_483; B7/2015_484; B7/2015_485; B7/2015_486; B7/2015_487; B7/2015_488; B7/2015_489; B7/2015_490; B7/2015_491; B7/2015_492; Bjarni Saemundsson; CTD/Rosette; CTD-RO; Current velocity, east-west; Current velocity, north-south; DATE/TIME; Depth, bottom/max; DEPTH, water; Event label; KB2018614; KB2018614_633; KB2018614_634; KB2018614_635; KB2018614_636; KB2018614_637; KB2018614_638; KB2018614_639; KB2018614_640; KB2018614_641; KB2018614_642; KB2018614_643; KB2018614_644; KB2018614_645; KB2018614_646; KB2018614_647; KB2018614_648; KB2018614_649; KB2018614_650; KB2018614_651; KB2018614_652; KB2018614_653; KB2018614_654; KN203-2; KN203-2_108; KN203-2_109; KN203-2_110; KN203-2_111; KN203-2_112; KN203-2_113; KN203-2_114; KN203-2_115; KN203-2_116; KN203-2_117; KN203-2_118; KN203-2_119; KN203-2_120; KN203-2_121; KN203-2_122; KN203-2_123; KN203-2_124; KN203-2_125; KN203-2_127; KN203-2_128; KN203-2_129; KN203-2_130; KN203-2_131; KN203-2_132; KN203-2_133; KN203-2_134; KN203-2_135; KN203-2_143; KN203-2_144; KN203-2_145; KN203-2_146; KN203-2_147; KN203-2_148; KN203-2_149; KN203-2_150; KN203-2_151; Knorr; Kristine Bonnevie; LATITUDE; LONGITUDE; Lowered Acoustic Doppler Current Profiler (LADCP)

Type: Dataset

Format: text/tab-separated-values, 19650 data points

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Water velocity profiles in the transect Slétta from LADCP from several cruises (2019)

Semper, Stefanie ; Valdimarsson, Héðinn ; Pickart, Robert ; [et al.]

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Publication Date: 2023-03-02

Keywords: B1/2011; B1/2011_52; B1/2011_53; B1/2011_55; B1/2011_56; B1/2011_57; B1/2011_58; B1/2011_59; B1/2013; B1/2013_66; B1/2013_67; B1/2013_68; B1/2013_69; B1/2013_70; B1/2013_71; B1/2013_72; B1/2013_73; B1/2013_74; B10/2009; B10/2009_572; B10/2009_573; B10/2009_574; B10/2009_575; B10/2009_576; B10/2009_577; B10/2009_578; B10/2009_579; B10/2009_580; B10/2009_581; B10/2009_582; B10/2009_583; B10/2009_584; B10/2009_585; B10/2009_586; B11/2017; B11/2017_777; B11/2017_778; B11/2017_779; B11/2017_780; B11/2017_781; B11/2017_782; B11/2017_783; B11/2017_784; B11/2017_785; B2/2012; B2/2012_76; B2/2012_77; B2/2012_78; B2/2012_79; B2/2012_80; B2/2012_81; B2/2012_82; B2/2012_83; B7/2015; B7/2015_453; B7/2015_454; B7/2015_455; B7/2015_456; B7/2015_457; B7/2015_458; B7/2015_459; B7/2015_460; B7/2015_461; Bjarni Saemundsson; CTD/Rosette; CTD-RO; Current velocity, east-west; Current velocity, north-south; DATE/TIME; Depth, bottom/max; DEPTH, water; Event label; Håkon Mosby; HM2016618; HM2016618_889; HM2016618_890; HM2016618_891; HM2016618_892; HM2016618_893; HM2016618_894; HM2016618_895; HM2016618_896; HM2016618_897; HM2016618_898; HM2016618_899; HM2016618_900; HM2016618_901; HM2016618_902; HM2016618_903; HM2016618_904; HM2016618_905; HM2016618_906; HM2016618_907; KB2018614; KB2018614_615; KB2018614_617; KB2018614_618; KB2018614_619; KB2018614_620; KB2018614_621; KB2018614_622; KB2018614_623; KB2018614_624; KB2018614_625; KB2018614_626; KB2018614_627; KB2018614_628; KB2018614_629; KB2018614_630; KB2018614_631; KB2018614_632; KN203-2; KN203-2_158; KN203-2_159; KN203-2_160; KN203-2_161; KN203-2_162; KN203-2_163; KN203-2_164; KN203-2_165; KN203-2_166; KN203-2_167; KN203-2_168; KN203-2_169; KN203-2_170; KN203-2_171; KN203-2_172; Knorr; Kristine Bonnevie; LATITUDE; LONGITUDE; Lowered Acoustic Doppler Current Profiler (LADCP); MULT; Multiple investigations

Type: Dataset

Format: text/tab-separated-values, 22828 data points

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X-ray diffraction (XRD) measurements and stable isotopes of rock-sediment sample GeoB11319-1 (2019)

Tamborrino, Leonardo ; Himmler, Tobias ; Elvert, Marcus ; [et al.]

PANGAEA

In: Supplement to: Tamborrino, Leonardo; Himmler, Tobias; Elvert, Marcus; Conti, Daniel; Gualtieri, Alessandro F; Fontana, Daniela; Bohrmann, Gerhard (2019): Formation of tubular carbonate conduits at Athina mud volcano, eastern Mediterranean Sea. Marine and Petroleum Geology, 107, 20-31, https://doi.org/10.1016/j.marpetgeo.2019.05.003

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Publication Date: 2023-03-03

Description: Tubular carbonate conduits (TCC) represent the termination of fluid plumbing systems in environments of hydrocarbon seepage and play a relevant role in the discharge of methane from sub-seafloor sediments to the water column. However, the biogeochemical reactions and biological activities involved in their formation are not fully understood. To address this, TCC samples were collected with a remotely operated vehicle from the seabed on the SW flank of the Athina mud volcano in the eastern Mediterranean Sea. Petrographic, mineralogical, stable carbon and oxygen isotope and lipid biomarker analyses were performed to elucidate the formation processes of the tubular carbonates. Clotted and fibrous aragonite form the internal lining of the cavities, while the outer portion of the tubes is formed by micritic Mg-calcite cementing hemipelagic sediment. 13C-depleted Mg-calcite and aragonite (as low as −14.4‰ V-PDB) and lipid biomarkers (archaeol, −89.8‰ V-PDB) indicate that carbonate precipitation was influenced by sulfate-dependent anaerobic oxidation of methane (AOM). AOM locally enhances aragonite precipitation, thereby facilitating early lithification of the conduits within the mud volcano sediments. The size and morphology of the TCC comparable with the buried portion of tubeworm colonies found in the proximity of the sampling site. However, our results suggest that TCC likely formed by the action of burrowing organism rather than being mineralizations of the tubeworm colonies. This study provides new insights into the interpretation and understanding of TCC, highlighting the role of macrofaunal activity in the formation of migration pathways for hydrocarbon-rich fluids on the flank of a mud volcano.

Keywords: Center for Marine Environmental Sciences; MARUM

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Format: application/zip, 2 datasets

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Pollen percentages, Charcoal flux, Mg/Ca-based SST and Benthic foraminiferal δ18O records of site GeoB16602 (2019)

Cheng, Zhongjing ; Weng, Chengyu ; Steinke, Stephan ; [et al.]

PANGAEA

In: Supplement to: Cheng, Zhongjing; Weng, Chengyu; Steinke, Stephan; Mohtadi, Mahyar (2018): Anthropogenic modification of vegetated landscapes in southern China from 6,000 years ago. Nature Geoscience, 11, 939-943, https://doi.org/10.1038/s41561-018-0250-1

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Publication Date: 2023-03-03

Description: Vegetation dynamics during previous warm interglacial periods shed light on the human impacts on natural ecosystems during the Holocene. However, reliable terrestrial records that span such periods are rare and provide little information on regional scale. Here we present a high-resolution marine pollen record from the northern South China Sea, which reveals that during five peak interglacial periods, Marine Isotope Stages 13a, 11c, 9c, 5e and 1 (the Holocene), the vegetation successions in southern China were similar. At the beginning of each interglacial period, tropical rainforest conifers, which include Dacrydium, Dacrycarpus and Podocarpus, and associated broadleaved taxa, such as Altingia, expanded quickly at the expense of the subtropical/temperate montane conifer Pinus. Near the end of the warm periods, Pinus recovered and the tropical taxa retreated. However, the Holocene displays subtle but significant differences in which the species turnover was interrupted and the rainforest conifers did not fully expanded. The Mg/Ca-based sea surface temperature record from the same site reveals that temperature was the major control of the rise and fall of the peak interglacial vegetation. However, exceptionally high charcoal fluxes during the Holocene suggest that human activities through land-use modifications completely, and possibly permanently, altered the natural vegetation trend five to six thousand years ago.

Keywords: Center for Marine Environmental Sciences; MARUM

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Format: application/zip, 5 datasets

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Holocene bulk and n-alkane organic geochemical proxies from cores MD05-2905 and GeoB16601-5 from the Northern South China Sea (2019)

Contreras-Rosales, Lorena Astrid ; Jennerjahn, Tim C ; Steinke, Stephan ; [et al.]

PANGAEA

In: Supplement to: Contreras-Rosales, Lorena Astrid; Jennerjahn, Tim C; Steinke, Stephan; Mohtadi, Mahyar; Schefuß, Enno (2019): Holocene changes in biome size and tropical cyclone activity around the Northern South China Sea. Quaternary Science Reviews, 215, 45-63, https://doi.org/10.1016/j.quascirev.2019.05.004

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Publication Date: 2023-03-03

Description: The South China Sea (SCS), characterized by a large continental shelf, is located at the edge of the Asian monsoon domain. In this study, two marine sediment cores from the northern SCS (NSCS) continental slope were investigated to construct composite vegetation and precipitation isotopic composition records based on the δ13C and δD values of plant-wax n-alkanes throughout the Holocene (last 11,200 years; i.e. 11.2 ka). The composite δ13Cwax record indicates an overall predominance of C3 vegetation over the last 11.2 ka. Before 8 ka BP, higher δ13Cwax values are attributed to preferential wax input from grassland and wetland biomes on the exposed continental shelf. After the inundation of the shelf by eustatic sea level rise until ca. 8 ka BP grassland and wetland biomes suffered a major size reduction and arboreal vegetation became better represented in the δ13Cwax record. The composite temperature corrected δDwax-T record suggests that moisture source variability drove precipitation isotopic composition changes during the Holocene. Lower δDwax-T values before 8.3 ka BP are interpreted as a larger moisture contribution by Pacific Ocean tropical cyclones, whereas higher δDwax-T values after 8.5 ka BP are interpreted as a larger moisture contribution from the Indian Ocean summer monsoon. Higher incidence of tropical cyclones in the NSCS during the Early Holocene was related to a temporary westward shift of the Western Pacific Warm Pool and enhanced insolation over the Northern Hemisphere. Both external and internal forcing mechanisms regulated moisture source changes in East Asia during the Holocene.

Keywords: Center for Marine Environmental Sciences; Leibniz Centre for Tropical Marine Research; MARUM; ZMT

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Format: application/zip, 5 datasets

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A continuous biomass‐burning record based on the fire biomarker levoglucosan of sediment core GeoB9528-3 (2019)

Schreuder, Laura T ; Hopmans, Ellen C ; Castañeda, Isla S ; [et al.]

PANGAEA

In: Supplement to: Schreuder, Laura T; Hopmans, Ellen C; Castañeda, Isla S; Schefuß, Enno; Mulitza, Stefan; Sinninghe Damsté, Jaap S; Schouten, Stefan (2019): Late Quaternary biomass burning in Northwest Africa and interactions with climate, vegetation, and humans. Paleoceanography and Paleoclimatology, 34(2), 153-163, https://doi.org/10.1029/2018PA003467

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Publication Date: 2023-03-03

Description: Biomass burning on the African continent is widespread and interactions with climate, vegetation dynamics and biogeochemical cycling are complex. To obtain a better understanding of these complex relationships, African fire history has been widely studied, although mostly on relatively short time-scales (i.e. yrs to kyrs) and less commonly on long-term scales. Here, we present a 192-kyr, continuous biomass-burning record from sub-Saharan Northwest Africa based on the fire biomarker levoglucosan in a marine sediment core offshore Guinea. Notable features of our record include an increase in levoglucosan accumulation at 80 ka and two peaks at 50-60 ka. The event at 80 ka is likely related to an overall increase in sedimentation rates rather than an increase in biomass burning in the Northwest African savanna region. Our record indicates that glacial/interglacial changes in regional climate and vegetation composition (C3 vs. C4 plants) were not a major influence on biomass burning over the last 192 kyrs. However, we suggest that the burning events at 50-60 ka might be caused by increased occurrence of C3 vegetation and human settlement in this region. At this time, the savanna region became wetter and fuel loads likely increased. Therefore, the region was more hospitable for humans, who likely used fire for hunting activities. Collectively, we hypothesize that on longer (glacial/interglacial) timescales, biomass burning, regional climate and African vegetation are not necessarily coupled, while around 50-60 ka, higher fuel loads and human fire-use may have influenced fire occurrence in sub-Saharan Northwest Africa.

Keywords: Carbon; Center for Marine Environmental Sciences; charcoal; fire history; indicators; levoglucosan; MARUM; Monsoon; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; organic aerosols; preservation; record; sediments

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Format: application/zip, 2 datasets

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Planktic foraminiferal Mg/Ca, Nd/Ca and oxygen isotopes and XRF core scanner data (Ti/Ca) of sediment core GeoB17419-1 (2019)

Hollstein, Martina ; Mohtadi, Mahyar ; Rosenthal, Yair ; [et al.]

PANGAEA

In: Supplement to: Hollstein, Martina; Mohtadi, Mahyar; Rosenthal, Yair; Prange, Matthias; Oppo, Delia W; Martínez Méndez, Gema; Tachikawa, Kazuyo; Moffa-Sanchez, Paola; Steinke, Stephan; Hebbeln, Dierk (2018): Variations in Western Pacific Warm Pool surface and thermocline conditions over the past 110,000 years: Forcing mechanisms and implications for the glacial Walker circulation. Quaternary Science Reviews, 201, 429-445, https://doi.org/10.1016/j.quascirev.2018.10.030

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Publication Date: 2023-03-03

Description: Surface and thermocline conditions of the Western Pacific Warm Pool (WPWP) reflect changes in regional and basin scale ocean and atmosphere circulations and in turn may affect climate globally. Previous studies suggest that a range of factors influences the WPWP on different timescales, however the precise forcings and mechanisms are unclear. Combining surface and thermocline records from sediment cores offshore Papua New Guinea we explore the influence of local and remote processes on the WPWP in response to astronomical forcing and changing glacial-interglacial boundary conditions over the past 110 kyr. We find that thermocline temperatures change with variations in Earth's obliquity with higher temperatures coinciding with high obliquity, which is attributed to variations in subduction and advection of the South Pacific Tropical Water. In contrast, rainfall variations associated with meridional migrations of the Intertropical Convergence Zone are primarily driven by changes in insolation due to precession. Records of bulk sedimentary Ti/Ca and foraminiferal Nd/Ca indicate an additional influence of obliquity, which, however, cannot unambiguously be related to changes in precipitation. Finally, our results suggest a thermocline deepening during the Last Glacial Maximum (LGM). A compilation of available proxy records illustrates a dipole-like pattern of LGM thermocline depth anomalies with a shoaling (deepening) in the northern (southern) WPWP. A comparison of the proxy compilation with an ensemble of Paleoclimate Model Intercomparison Project (PMIP) climate model simulations reveals that the spatial pattern of LGM thermocline depth anomalies is mainly attributable to a contraction of the Pacific Walker circulation on its western side.

Keywords: Center for Marine Environmental Sciences; MARUM

Type: Dataset

Format: application/zip, 4 datasets

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Sediment analyses of sediment cores from the cold-water coral mound province off Melilla, southern Alboran Sea (2019)

Wang, Haozhuang ; Lo Iaconob, Claudio ; Wienberg, Claudia ; [et al.]

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In: Supplement to: Wang, Haozhuang; Lo Iaconob, Claudio; Wienberg, Claudia; Titschack, Jürgen; Hebbeln, Dierk (2019): Cold-water coral mounds in the southern Alboran Sea (western Mediterranean Sea): Internal waves as an important driver for mound formation since the last deglaciation. Marine Geology, 412, 1-18, https://doi.org/10.1016/j.margeo.2019.02.007

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Publication Date: 2023-03-03

Description: Cold-water corals (CWCs) are widely distributed in the entire Alboran Sea (western Mediterranean Sea), but only along the Moroccan margin they have formed numerous coral mounds, which are constrained to the West and the East Melilla CWC mound provinces (WMCP and EMCP). While information already exists about the most recent development of the coral mounds in the EMCP, the temporal evolution of the mounds in the WMCP was unknown up to the present. In this study, we present for the first time CWC ages obtained from four sediment cores collected from different mounds of the WMCP, which allowed to decipher their development since the last deglaciation. Our results revealed two pronounced periods of coral mound formation. The average mound aggradation rates were of 75-176 cm kyr-1 during the Bølling-Allerød interstadial and the Early Holocene, only temporarily interrupted during the Younger Dryas, when aggradation rates decreased to 〈45 cm kyr-1. Since the Mid Holocene, mound formation significantly slowed-down and finally stagnated until today. No living CWCs thrive at present on the mounds and some mounds became even buried. The observed temporal pattern in mound formation coincides with distinct palaeoceanographic changes that significantly influenced the local environment. Within the Alboran Sea, enhanced surface ocean productivity and seabed hydrodynamics prevailed during the Bølling-Allerød and the Early Holocene. Only with the onset of the Mid Holocene, the area turned into an oligotrophic setting. The strong hydrodynamics during the mound formation periods are most likely caused by internal waves that developed along the water mass interface between the Modified Atlantic Water and the Levantine Intermediate Water. In analogue to observations from modern CWC settings, we assume that internal waves created turbulent hydrodynamic conditions that increased the lateral delivery of particulate material, promoting the availability of food for the sessile CWCs. Overall, our data point to the dominant role of the water column structure in controlling the proliferation of CWCs and hence the development of coral mounds in the southern Alboran Sea.

Keywords: Alboran Sea; Center for Marine Environmental Sciences; Cold-water coral mounds; coral mound formation; internal waves; last deglaciation; Levantine Intermediate Water; MARUM; mound aggradation rate

Type: Dataset

Format: application/zip, 15 datasets

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Radiocarbon dating, grain size analyses, and XRF data on sediments from the Hauraki Gulf, New Zealand (2019)

Hebbeln, Dierk ; Boxberg, Florian

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In: Supplement to: Boxberg, Florian; Blossier, Brice; de Lange, Willem P; Fox, Bethany R Storrs; Hebbeln, Dierk (2020): Sediment deposition in the central Hauraki Gulf, New Zealand. Geo-Marine Letters, 40(2), 227-241, https://doi.org/10.1007/s00367-019-00583-1

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Publication Date: 2023-03-03

Description: Based on the analysis of 14 short sediment cores, we present new insights into the distribution of surficial sediments in the central Hauraki Gulf, a semi-enclosed coastal embayment on the northeast coast of New Zealand's North Island. We identify and discuss the effects of interaction of modern wind-generated waves and currents with regard to deposition and reworking of sediments in the Gulf. The modern hydrodynamic regime is controlled by tidal currents, oceanic inflows, and wave-induced currents and it is responsible for a N-S gradient in sediment texture and elemental concentrations in the central Hauraki Gulf sediments. The present-day sediment input into the system is generally low and consists of fine-grained fluvial sediments mostly deposited in the southern study area and comparatively high inputs of relict carbonate material to the northern study sites. The central Hauraki Gulf sediments, which show numerous age reversals in the sedimentary record, can be characterised as palimpsest sediments, as a consequence of continuous reworking and storm-induced sediment transport. In view of the new data, a previously assumed significant post-transgression accumulation of sediments of 〉 10 m in the central Hauraki Gulf appears to be very unlikely.

Keywords: Center for Marine Environmental Sciences; Grain size data; Hauraki Gulf; INTERCOAST; MARUM; New Zealand; Radiocarbon datings; XRF data

Type: Dataset

Format: application/zip, 3 datasets

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B isotope ratios of hydrothermal fluids and volcanic rocks from the Manus Basin and New Hebrides ridge (2019)

Wilckens, Frederike Kristina ; Reeves, Eoghan P ; Bach, Wolfgang ; [et al.]

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Publication Date: 2023-03-03

Description: The dataset contains boron (B) concentrations and isotope ratios of hydrothermal vent fluids and volcanic rocks from different vent fields within the Manus Basin, Papua New Guinea, and Nifonea volcano, New Hebrides back-arc. The fluids from these settings show a range of salinities, gas contents, acidities, and host rock compositions; many of them are influenced by phase separation and by addition of magmatic volatiles (both CO2 and SO2). Previous studies of hydrothermal vents in arc/back-arc settings suggest that B contents and isotopic composition of vent fluids are controlled by interactions between seawater, basement and sediments, and propose that phase separation and magmatic fluids play only a subordinate role. In our study, we demonstrate that vent fluids with minor magmatic input indeed reflect the interaction between seawater and oceanic crust. In contrast, the low-salinity Nifonea fluids and some of the acid-sulfate fluids from the Manus Basin have higher B contents as expected, whereas other volatile-rich fluids from the Manus Basin show B depletions. The lack of correlation between B contents and the intensity of magmatic fluid influx (CO2 and SO2) may indicate that magma degassing is not responsible for the B enrichments or depletions in these vent fluids. B enrichments might be related to preferential partitioning of B into the vapour phase during phase separation under PT-conditions well above the two-phase curve and critical line (i.e. T 〉〉 Tcritical, P 〉〉 Pcritical). However, this cannot explain the low B concentrations in the vapour-rich vent fluids from the Manus Basin and the low B isotope ratios in the Nifonea fluids. Instead, we propose that B concentrations and isotope ratios in submarine vent fluids largely depend on the residence and reaction time of the vent fluid in the subsurface. In general, all vent fluids are still influenced by water-rock interaction during hydrothermal circulation. However, vent fluids with short residence times define a trend towards lower B concentrations and isotope ratios, which can be explained by mixing between hydrothermal and magmatic fluid, which is similar to the composition of the host rock. In contrast, the B signature of the magmatic fluid can be overprinted due to preferential mobilization of B from the oceanic crust into vapour-rich fluids at longer reaction times. Thus, B may provide a tool for estimating the extent of B leaching and hence hydrothermal alteration in the subseafloor.

Keywords: arc; back-arc; basalt; B isotope; boron isotopes; Center for Marine Environmental Sciences; hydrothermal; magmatic degassing; MARUM; phase separation; vent fluids

Type: Dataset

Format: application/zip, 2 datasets

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HydroC pCO2 measurements during Celtic Explorer cruise CE12010 at station 44ROV12 (Gas Release Experiment) (2019)

Vielstädte, Lisa ; Linke, Peter ; Schmidt, Mark

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Publication Date: 2023-03-03

Description: Raw data of pCO2 measurements during Celtic Explorer cruise CE12010 at station 44ROV12 (Gas Release Experiment). The gas discharge of the gas release experiment was observed in situ during a 4 hour dive with GEOMAR's remotely operated vehicle ROV Kiel 6000 equipped with HD camera/video device and a sonar system. The spread of the dissolved CO2 plume was monitored geochemically using the commercial HydroC pCO2 sensor (S/N 0412-006, Kongsberg Maritime Contros GmbH) mounted to the front porch of the ROV. The sensor was calibrated for pCO2 signals up to 3,000 µatm (accuracy ~1% of reading resolution; resolution: 〈30 µatm) and was programmed to measure in 60 s intervals, which is equal to the sensor's response time.

Keywords: 44ROV12; carbon dioxide; Carbon dioxide, partial pressure; CE12010; CE12010_44; Celtic Explorer; Conductivity; CTD, SEA-BIRD SBE 9 plus; DATE/TIME; Density, mass density; DEPTH, water; ECO2; gas release experiment; geological storage; HydroC pCO2 sensor, CONTROS; Identification; LATITUDE; leakage; LONGITUDE; North Sea; Remote operated vehicle; ROV; Salinity; Sleipner; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Temperature, water

Type: Dataset

Format: text/tab-separated-values, 2238 data points

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Experimental data of sediment bed behaviour in a current (2019)

Staudt, Franziska ; Mullarney, Julia C ; Pilditch, Conrad A ; [et al.]

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In: Supplement to: Staudt, Franziska; Mullarney, Julia C; Pilditch, Conrad A; Huhn, Katrin (2019): Effects of grain‐size distribution and shape on sediment bed stability, near‐bed flow and bed microstructure. Earth Surface Processes and Landforms, 44(5), 1100-1116, https://doi.org/10.1002/esp.4559

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Publication Date: 2023-03-03

Description: This data set has been collected in annular flume experiments with bimodal sand mixtures at the University of Waikato, New Zealand. Medium sand (D50,c = 400 µm) was mixed with 40 % fine material of different diameters (D50,f = 53; 111; 193 µm) and subjected to increasing flow velocities (U = 1.3-22.2 cm/s). The near-bed hydrodynamics, the bed level and the suspended sediment concentration were investigated. In the affiliated publication (DOI: 10.1002/esp.4559) selected results are compared with results from similar tests with glass beads. This data set comprises: 1) grain-size distributions of the sand mixtures ("GrainSizeDistr_N") and glass beads ("GrainSizeDistr_GB") 2) averaged flow velocity profiles in m/s ("N_RD_number_Uxy_interval" and "GB_RD_Uxy_interval") 3) detailed timeseries of the bed level in m below the ADV profiler ("N_RD_number_Bottom") 4) suspended sediment concentrations in mg/l ("N_RD_number_SSC") "RD" is a measure for the grain-size distribution of the mixture (see publication). The experiments with natural sand (N) were repeated three times, the "number" of the experiment is indicated in the file names. For experiment N_77 only the data of the 3rd replication is provided. Every experiment comprised 12 "intervals" with increasing flow velocities. For each interval the averaged flow velocity profile is provided. Please refer to DOI: 10.1002/esp.4559 for further information about instrumentation etc.

Keywords: Center for Marine Environmental Sciences; File content; File format; File name; File size; MARUM; Uniform resource locator/link to file

Type: Dataset

Format: text/tab-separated-values, 20 data points

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M84/4 raw data of EM710 multibeam echosounder (bathymetry & beam time series) (2019)

Hanebuth, Till J J ; Schwenk, Tilmann ; Lenhart, Antje ; [et al.]

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Publication Date: 2023-03-03

Description: Bathymetry data was acquired during R/V METEOR cruise M84/4 at the Galician Shelf off Northwest Spain in the Northeast Atlantic between 01.05.2011 and 28.05.2011. The main objectives of the cruise were the investigation of sediment transport processes from shallow to deep waters, understanding sediment dynamics, analysis of material downslope processes and the reconstruction of modern and past environmental conditions. The cruise comprised seismic, sedimentological, magnetic, geochemical and palaeoceanographic methods. Extensive bathymetric mapping during M84/4 based on the multibeam echosounders (MBES) KONGSBERG EM710 and EM122 provided the basis for sediment coring and additional investigations. Hydroacoustic data revealed the diverse morphology in the study area, driven by both sedimentary and tectonic processes, including contouritic deposits, slope gullies, canyon/channel systems, ridges and seamounts. The sub-bottom profiler PARASOUND, multichannel seismics, ADCP, several coring devices and the electromagnetic profiler MARUM-NERIDIS III complemented the research programme of the cruise. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval. Description of the data source: During the M84/4 cruise, the hull-mounted KONGSBERG EM710 multibeam echosounder (MBES) was utilized to perform bathymetric mapping of high resolution in water depths of 3 m to – theoretically – 2000 m. Best quality data is, however, achieved in water depths of less than 600 m, and in rough weather conditions less than 400 m. The EM710 operates at sonar frequencies of 70 to 100 kHz. Three sectors divide the transmit fan, where distinct frequencies or waveforms are transmitted sequentially. The swath width can reach 5.5 times the water depth. 256 beams with an acoustical 1°(TX)/1°(RX) footprint are formed for each ping. The transmit fan is electronically stabilized for roll, pitch and yaw. Combining phase and amplitude bottom detection algorithms allows achieving best possible accuracy. For further information, consult: https://epic.awi.de/id/eprint/26726/1/Kon2007b.pdf. The position and depth of the water column is estimated for each beam by using the detected two-way-travel time and the beam angle known for each beam and taking ray bending due to refraction in the water column by sound speed into account. During the M84/4 cruise, the EM710 was running in a 24-hour watch mode, in addition to the EM122 and the PARASOUND sub-bottom profiling system. Acquisition of EM710 data was reliable during the whole cruise; however, problems occurred during rough weather conditions, since the EM710 lost the bottom signal in depths of more than 400 m. Responsible person during this cruise / PI: Tilmann Schwenk (tschwenk@marum.de) Chief Scientist: Till J. J. Hanebuth (thanebuth@coastal.edu) CR: https://www.tib.eu/de/suchen/id/awi%3Adoi~10.2312%252Fcr_m84_4/ CSR: https://www.ldf.uni-hamburg.de/meteor/wochenberichte/wochenberichte-meteor/m84/m84-4-scr.pdf

Keywords: Bathymetry; Center for Marine Environmental Sciences; CT; EM710; File format; File name; File size; Galician Shelf; hydroacoustics; M84/4; M84/4-track; MARUM; Meteor (1986); Northeast Atlantic; Seismic; Underway cruise track measurements; Uniform resource locator/link to file

Type: Dataset

Format: text/tab-separated-values, 3192 data points

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NavCleaner (OFOS Edition) for processing raw Posidonia USBL datagrams (2019)

Marcon, Yann

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Publication Date: 2023-03-03

Description: The NavCleaner (OFOS Edition) is a program that filters, smooths and interpolates USBL navigation data. The NavCleaner (OFOS Edition) is optimised to process the navigation tracks of the AWI OFOS and OFOBS instruments but it can be used to process Posidonia USBL data from other instruments as well. As input it only requires a text file containing raw USBL datagrams. The program outputs comma-separated files containing the filtered, smoothed and 1 Hz interpolated navigation timeseries (both geographic coordinates and UTM/UPS coordinates). All calculations are done internally on projected coordinates using the most relevant WGS84 UTM/UPS zone in order to minimize errors. If used with the OFOS / OFOBS platforms, the NavCleaner (OFOS Edition) can optionally read and interpolate the altimeter data from the photos' EXIF metadata, and compute the coordinates for every photo as well as for every observations in the dive report (Excel format). A dive report template is provided, which can also be used with other platforms.

Keywords: acoustic; Center for Marine Environmental Sciences; dive track; interpolation; MARUM; Navigation; OFOS; Posidonia; positioning; PTSAG; track; USBL

Type: Dataset

Format: application/zip, 566.8 MBytes

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NavCleaner for processing USBL, DVL and hybrid dive tracks (2019)

Marcon, Yann

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Publication Date: 2023-03-03

Description: NavCleaner is a program to filter, smooth and interpolate underwater navigation data (USBL, DVL, hybrid). NavCleaner is optimised to process the navigation data of the MARUM ROV QUEST4000 but it can be used to process dive track data from other instruments as well. All calculations are done internally on projected coordinates using the most relevant WGS84 UTM/UPS zone in order to minimize errors. As inputs, NavCleaner can read USBL, DVL, depth, altitude (height above bottom), heading, pitch, and roll data timeseries. A configuration file enables NavCleaner to read a variety of text file formats. The program outputs comma-separated files containing the filtered, smoothed and 1 Hz interpolated navigation timeseries (both geographic coordinates and UTM/UPS coordinates) for all input data timeseries. If both USBL and DVL data are used as inputs, NavCleaner also merges the USBL and DVL data to create a hybrid navigation track. Optionally, NavCleaner can compute the coordinates for every observations in the dive report (Excel format).

Keywords: acoustic; AUV; Center for Marine Environmental Sciences; dive track; DVL; hybrid; interpolation; MARUM; Navigation; Posidonia; positioning; ROV; track; USBL

Type: Dataset

Format: application/zip, 547.6 MBytes

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Planktic foraminiferal test size and size normalised weight from IODP Hole 306-1313B and 306-1313C during the Pliocene (2019)

Todd, Chloe ; Schmidt, Daniela N ; Robinson, Marci M ; [et al.]

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Publication Date: 2023-02-24

Keywords: 306-1313B; 306-1313C; AGE; Core; CORE; Counting, foraminifera; DEPTH, sediment/rock; Diameter; DSDP/ODP/IODP sample designation; Event label; Foraminifera; Fragmentation; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Percentile 95; Sample code/label; Sea surface temperature; Size normalized weight; SST calculated from alkenones

Type: Dataset

Format: text/tab-separated-values, 974 data points

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