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  • 1
    Publication Date: 2019-07-31
    Description: Variability of surface water masses of the Laptev and the East-Siberian seas in August–September 2018 is studied using in situ and satellite data. In situ data was collected during ARKTIKA-2018 expedition and then completed with satellite estimates of sea surface temperature (SST) and salinity (SSS), sea surface height, satellite-derived wind speeds and sea ice concentrations. Derivation of SSS is still challenging in high latitude regions, and the quality of Soil Moisture and Ocean Salinity (SMOS) SSS retrieval was improved by applying a threshold on SSS weekly error. The validity of SST and SSS products is demonstrated using ARKTIKA-2018 continuous thermosalinograph measurements and CTD casts. The surface gradients and mixing of river and sea waters in the free of ice and ice covered areas is described with a special attention to the marginal ice zone. The Ekman transport was calculated to better understand the pathway of surface water displacement. T-S diagram using surface satellite estimates shows a possibility to investigate the surface water masses transformation in detail.
    Print ISSN: 1812-0806
    Electronic ISSN: 1812-0822
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 2
    Publication Date: 2021-02-04
    Description: Variability of surface water masses of the Laptev and the East Siberian seas in August–September 2018 is studied using in situ and satellite data. In situ data were collected during the ARKTIKA-2018 expedition and then complemented with satellite-derived sea surface temperature (SST), salinity (SSS), sea surface height, wind speed, and sea ice concentration. The estimation of SSS fields is challenging in high-latitude regions, and the precision of soil moisture and ocean salinity (SMOS) SSS retrieval is improved by applying a threshold on SSS weekly error. For the first time in this region, the validity of DMI (Danish Meteorological Institute) SST and SMOS SSS products is thoroughly studied using ARKTIKA-2018 expedition continuous thermosalinograph measurements and conductivity–temperature–depth (CTD) casts. They are found to be adequate to describe large surface gradients in this region. Surface gradients and mixing of the river and the sea water in the ice-free and ice-covered areas are described with a special attention to the marginal ice zone at a synoptic scale. We suggest that the freshwater is pushed northward, close to the marginal ice zone (MIZ) and under the sea ice, which is confirmed by the oxygen isotope analysis. The SST-SSS diagram based on satellite estimates shows the possibility of investigating the surface water mass transformation at a synoptic scale and reveals the presence of river water on the shelf of the East Siberian Sea. The Ekman transport is calculated to better understand the pathway of surface water displacement on the shelf and beyond.
    Print ISSN: 1812-0784
    Electronic ISSN: 1812-0792
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 3
    Publication Date: 2022-01-07
    Description: Variability of surface water masses of the Laptev and the East Siberian seas in August–September 2018 is studied using in situ and satellite data. In situ data were collected during the ARKTIKA-2018 expedition and then complemented with satellite-derived sea surface temperature (SST), salinity (SSS), sea surface height, wind speed, and sea ice concentration. The estimation of SSS fields is challenging in high-latitude regions, and the precision of soil moisture and ocean salinity (SMOS) SSS retrieval is improved by applying a threshold on SSS weekly error. For the first time in this region, the validity of DMI (Danish Meteorological Institute) SST and SMOS SSS products is thoroughly studied using ARKTIKA-2018 expedition continuous thermosalinograph measurements and conductivity–temperature–depth (CTD) casts. They are found to be adequate to describe large surface gradients in this region. Surface gradients and mixing of the river and the sea water in the ice-free and ice-covered areas are described with a special attention to the marginal ice zone at a synoptic scale. We suggest that the freshwater is pushed northward, close to the marginal ice zone (MIZ) and under the sea ice, which is confirmed by the oxygen isotope analysis. The SST-SSS diagram based on satellite estimates shows the possibility of investigating the surface water mass transformation at a synoptic scale and reveals the presence of river water on the shelf of the East Siberian Sea. The Ekman transport is calculated to better understand the pathway of surface water displacement on the shelf and beyond.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2023-10-28
    Description: A standard Sea-Bird Electronics Inc SBE911+ CTD system with single temperature and conductivity sensors was used to measure temperature, conductivity and pressure at 73 stations during an expedition to the Laptev and East Siberian Seas in September-October 2019 aboard the research vessel Professor Multanovskiy. To measure chlorophyll content in the water, a pumped WETLabs WETStar fluorometer was connected to the SBE911+ system. Additionally, a Seabird 19plus V CTD with a pumped fluorescence sensor (WETStar) was mounted in the rosette frame to measure the fluorescence of dissolved organic matter (fDOM). Salinity and temperature data from the SBE 19plus V2 CTD are also part of the data set. We followed the manufacturer's recommendation to calculate salinity using Seabird processing software. Salinity is reported as practical salinity (PSU). Data were averaged at depth intervals of 1 m. Data are from the 2019 Transarktika Expedition (Leg 4/2 from Murmansk to Vladivostok), an initiative of the Russian Antarctic and Arctic Research Institute (AARI), carried out in collaboration with the Russian-German CATS project and funded by Minobrnauki (CATS RFMEFI61619X0108) and BMBF (CATS 03F0831B).
    Keywords: Arctic Ocean; Calculated; CATS; CATS - The Changing Arctic Transpolar System; Conductivity; CTD, Sea-Bird, SBE 19 Plus V2; CTD, Sea-Bird, SBE 19 Plus V2; measured with Fluorometer, WETStar; CTD, Sea-Bird, SBE 911plus; CTD, Sea-Bird, SBE 911plus; measured with Fluorometer, WETStar; CTD/Rosette; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Dissolved Organic Matter; East Siberian Sea; ELEVATION; Event label; Fluorescence, chlorophyll; Fluorescence, dissolved organic matter; Laptev Sea; Laptev Sea System; LATITUDE; LONGITUDE; LSS; Number of scans; PM19086-1; PM19087-1; PM19093-1; PM19094-1; PM19095-1; PM19096-1; PM19097-1; PM19100-1; PM19100-2; PM19104-1; PM19107-1; PM19109-1; PM19111-1; PM19111-2; PM19113-1; PM19115-1; PM19117-1; PM19119-1; PM19120-1; PM19122-1; PM19123-1; PM19124-1; PM19125-1; PM19127-1; PM19129-1; PM19131-1; PM19133-1; PM19135-1; PM19137-1; PM19139-1; PM19140-1; PM19160-1; PM19161-1; PM19162-1; PM19163-1; PM19164-1; PM19165-1; PM19166-1; PM19167-1; PM19168-1; PM19169-1; PM19170-1; PM19171-1; PM19172-1; PM19173-1; PM19174-1; PM19175-1; PM19176-1; PM19177-1; PM19178-1; PM19179-1; PM19180-1; PM19181-1; PM19182-1; PM19183-1; PM19184-1; PM19185-1; PM19186-1; PM19187-1; PM19188-1; PM19189-1; PM19190-1; PM19191-1; PM19192-1; PM19193-1; PM19194-1; PM19195-1; PM19196-1; PM19197-1; PM19198-1; PM19199-1; PM19200-1; PM19201-1; Pressure, water; Professor Multanovskiy; Salinity; shelf-basin transects; Temperature, water; Temperature, water, potential; Transarktika-2019_Leg4
    Type: Dataset
    Format: text/tab-separated-values, 139715 data points
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  • 5
    Publication Date: 2023-10-28
    Description: A standard Sea-Bird Electronics SBE911+ CTD system with a temperature and conductivity sensor was used to measure temperature, conductivity, and pressure at 180 stations during the Russian-international expedition Transarktika-2019 Leg 1 in the Barents Sea in March-May 2019 aboard the research vessel Akademik Tryoshnikov. We followed the manufacturer's recommendation to calculate salinity using Seabird processing software. The salinity is reported as Practical Salinity (PSU). Data were averaged at depth ranges of 1 m. Data are provided by the Antarctic and Arctic Research Institute (AARI) and reprocessed at the Helmholtz Centre for Polar and Marine Research, Alfred Wegener Institute. The Transarktika-2019 expedition was made possible by funding from the Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet). The scientific research was also supported by RFBR grants No. 18-05-60048 and 18-05-60083.
    Keywords: Akademik Tryoshnikov; Arctic Ocean; AT19001-1; AT19002-1; AT19004-1; AT19005-1; AT19006-1; AT19007-1; AT19008-1; AT19009-1; AT19010-1; AT19011-1; AT19012-1; AT19013-1; AT19014-1; AT19015-1; AT19016-1; AT19017-1; AT19018-1; AT19019-1; AT19020-1; AT19021-1; AT19022-1; AT19023-1; AT19024-1; AT19025-1; AT19026-1; AT19027-1; AT19028-1; AT19029-1; AT19030-1; AT19031-1; AT19032-1; AT19033-1; AT19034-1; AT19035-1; AT19036-1; AT19037-1; AT19038-1; AT19039-1; AT19040-1; AT19041-1; AT19042-1; AT19043-1; AT19044-1; AT19045-1; AT19046-1; AT19047-1; AT19048-1; AT19049-1; AT19050-1; AT19051-1; AT19052-1; AT19053-1; AT19054-1; AT19055-1; AT19056-1; AT19057-1; AT19058-1; AT19059-1; AT19060-1; AT19061-1; AT19062-1; AT19063-1; AT19064-1; AT19065-1; AT19066-1; AT19067-1; AT19068-1; AT19069-1; AT19070-1; AT19071-1; AT19072-1; AT19073-1; AT19074-1; AT19075-1; AT19076-1; AT19077-1; AT19078-1; AT19079-1; AT19080-1; AT19081-1; AT19082-1; AT19083-1; AT19084-1; AT19085-1; AT19086-1; AT19086-2; AT19086-3; AT19087-1; AT19088-1; AT19089-1; AT19089-2; AT19089-3; AT19090-1; AT19091-1; AT19092-1; AT19092-2; AT19092-3; AT19093-1; AT19094-1; AT19095-1; AT19095-2; AT19095-3; AT19096-1; AT19097-1; AT19098-1; AT19099-1; AT19100-1; AT19101-1; AT19102-1; AT19103-1; AT19104-1; AT19105-1; AT19106-1; AT19107-1; AT19108-1; AT19109-1; AT19110-1; AT19111-1; AT19112-1; AT19113-1; AT19114-1; AT19115-1; AT19116-1; AT19117-1; AT19118-1; AT19119-1; AT19120-1; AT19121-1; AT19122-1; AT19123-1; AT19124-1; AT19125-1; AT19126-1; AT19127-1; AT19128-1; AT19130-1; AT19131-1; AT19132-1; AT19133-1; AT19134-1; AT19135-1; AT19136-1; AT19137-1; AT19138-1; AT19139-1; AT19140-1; AT19141-1; AT19142-1; AT19148-1; AT19149-1; AT19150-1; AT19151-1; AT19152-1; AT19153-1; AT19154-1; AT19155-1; AT19156-1; AT19157-1; AT19158-1; AT19159-1; AT19160-1; AT19161-1; AT19162-1; AT19163-1; AT19164-1; AT19165-1; AT19166-1; AT19167-1; AT19168-1; AT19169-1; AT19170-1; AT19171-1; AT19172-1; AT19173-1; AT19174-1; AT19175-1; AT19176-1; AT19177-1; AT19178-1; AT19179-1; Barents Sea; Calculated; CATS; CATS - The Changing Arctic Transpolar System; Conductivity; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; DATE/TIME; Density, sigma-theta (0); DEPTH, water; ELEVATION; Event label; Ice drift experiment SEVERNYI POLYUS 2019; Kara Sea; LATITUDE; LONGITUDE; Number of scans; Pressure, water; Salinity; St. Anna Trough; Temperature, water; Temperature, water, potential; Transarktika-2019_Leg1
    Type: Dataset
    Format: text/tab-separated-values, 288309 data points
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  • 6
    Publication Date: 2024-01-24
    Description: A standard CTD system from Sea-Bird Electronics Inc SBE911+ with duplicate temperature and conductivity sensors was used to measure temperature, conductivity and pressure at 86 stations during an expedition to the Kara and Laptev Seas and the adjacent Arctic Ocean in August-September 2021 aboard the research vessel “Akademik Tryoshnikov”. We followed the manufacturer's recommendation to calculate salinity with Seabird processing software. The salinity is given as Practical Salinity (PSU). Data were averaged in depth bins of 1 m. The processed, but not bin-averaged, cnv-files from each station are also part of this publication (zip file). The accuracy of the conductivity sensors was verified by measurements on water samples with a salinometer. The data set published here includes only the data from the first conductivity (SN 3290) and temperature (SN 4127) sensors. Only at station 26 the data of the second sensor pair (SN 2618/Cond, SN 5115/Temp) were used. The CTD was connected to an SBE32 carousel water sampler with 24 12-liter bottles. Additionally, a Wetlabs ECO-AFL Fluorometer was connected to the SBE911+ system. The data are provided by the Arctic Century Expedition, a joint initiative led by the Swiss Polar Institute (SPI), the Antarctic and Arctic Research Institute (AARI) and GEOMAR Helmholtz Centre for Ocean Research Kiel (GEOMAR) and funded by the Swiss Polar Foundation, AARI, Minobrnauki (CATS RFMEFI61619X0108) and BMBF (CATS 03F0831).
    Keywords: Akademik Tryoshnikov; ArcticCentury; Arctic Century Expedition; Arctic Ocean; AT21; AT21_001-1; AT21_001-5; AT21_002-1; AT21_003-1; AT21_004-1; AT21_005-1; AT21_006-1; AT21_007-1; AT21_008-1; AT21_009-1; AT21_010-1; AT21_011-1; AT21_012-1; AT21_013-1; AT21_015-1; AT21_016-1; AT21_017-1; AT21_018-1; AT21_019-1; AT21_020-1; AT21_020-5; AT21_021-1; AT21_022-1; AT21_023-1; AT21_024-1; AT21_026-1; AT21_027-1; AT21_028-1; AT21_029-1; AT21_030-1; AT21_031-1; AT21_032-1; AT21_034-1; AT21_035-1; AT21_036-1; AT21_037-1; AT21_038-1; AT21_039-1; AT21_040-1; AT21_040-6; AT21_041-1; AT21_043-1; AT21_045-1; AT21_047-1; AT21_049-1; AT21_050-1; AT21_051-1; AT21_053-1; AT21_055-1; AT21_056-1; AT21_057-1; AT21_058-1; AT21_059-1; AT21_060-1; AT21_061-1; AT21_062-1; AT21_064-1; AT21_065-1; AT21_066-1; AT21_067-1; AT21_068-1; AT21_069-1; AT21_070-1; AT21_071-1; AT21_072-1; AT21_073-1; AT21_075-1; AT21_089-1; AT21_093-1; AT21_096-1; AT21_097-1; AT21_098-1; AT21_104-1; AT21_106-1; AT21_107-1; AT21_108-1; AT21_109-1; AT21_110-1; AT21_111-1; AT21_112-1; AT21_113-1; AT21_114-1; AT21_117-1; AT21_119-1; AT21_122-1; AT21_125-1; Barents Sea; Calculated; CATS; CATS - The Changing Arctic Transpolar System; Conductivity; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Fluorescence, chlorophyll; Fluorometer, WET Labs ECO AFL/FL; Kara Sea; Laptev Sea; Latitude of event; Longitude of event; Pressure, water; Salinity; shelf-basin transects; St. Anna Trough; Station label; Temperature, water; Temperature, water, potential
    Type: Dataset
    Format: text/tab-separated-values, 336264 data points
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  • 7
    Publication Date: 2024-02-27
    Description: A standard CTD system from Sea-Bird Electronics Inc SBE911+ with duplicate temperature and conductivity sensors was used to measure temperature, conductivity and pressure at 81 stations during an expedition to the Kara and Laptev Seas and the adjacent Arctic Ocean in August-September 2021 aboard the research vessel Akademik Tryoshnikov. We followed the recommendation of the manufacturer to calculate salinity with Seabird processing software. The salinity is given as Practical Salinity (PSU). The accuracy of the conductivity sensors was verified by measurements on water samples with a salinometer. The data set published here includes only the data from the first conductivity (SN 3290) and temperature (SN 4127) sensors. Only at station 26 the data of the second sensor pair (SN 2618/Cond, SN 5115/Temp) were used. The CTD was connected to a SBE32 Carousel Water Sampler with 24 12-liter bottles. Additionally, a Benthos Altimeter and a Wetlabs ECO-AFL Fluorometer were connected to the SBE911+ system. At 69 stations, 846 seawater samples were collected for analysis of dissolved inorganic nutrients (nitrate, nitrite, phosphate, ammonium, silicate), oxygen, total alkalinity, and pH. Dissolved inorganic nutrients were analyzed using a segmented flow analyzer from Seal Analytical. Ammonium was measured manually (colorimetric method) using a spectrophotometer (Shimadzu UV-1800). Dissolved oxygen was determined by the standard Winkler titration method using a Metrohm 916 TiTouch automatic titrator and a handheld titrator (BRAND). pH and total alkalinity were measured by potentiometric titration using an automatic titrator (Metrohm 916 TiTouch). The data are provided by the Arctic Century Expedition, a joint initiative led by the Swiss Polar Institute (SPI), the Antarctic and Arctic Research Institute (AARI) and GEOMAR Helmholtz Centre for Ocean Research Kiel (GEOMAR) and funded by the Swiss Polar Foundation, AARI, Minobrnauki (CATS RFMEFI61619X0108) and BMBF (CATS 03F0831).
    Keywords: Akademik Tryoshnikov; Alkalinity, total; Ammonium; ArcticCentury; Arctic Century Expedition; Arctic Ocean; AT21; AT21_001-5; AT21_002-1; AT21_003-1; AT21_004-1; AT21_005-1; AT21_006-1; AT21_007-1; AT21_008-1; AT21_009-1; AT21_010-1; AT21_012-1; AT21_013-1; AT21_015-1; AT21_016-1; AT21_017-1; AT21_018-1; AT21_019-1; AT21_020-1; AT21_020-5; AT21_022-1; AT21_023-1; AT21_024-1; AT21_026-1; AT21_027-1; AT21_028-1; AT21_029-1; AT21_030-1; AT21_031-1; AT21_032-1; AT21_034-1; AT21_035-1; AT21_036-1; AT21_037-1; AT21_038-1; AT21_039-1; AT21_040-1; AT21_040-6; AT21_041-1; AT21_043-1; AT21_045-1; AT21_047-1; AT21_049-1; AT21_050-1; AT21_051-1; AT21_053-1; AT21_055-1; AT21_057-1; AT21_058-1; AT21_059-1; AT21_060-1; AT21_061-1; AT21_062-1; AT21_064-1; AT21_065-1; AT21_066-1; AT21_067-1; AT21_068-1; AT21_069-1; AT21_070-1; AT21_071-1; AT21_072-1; AT21_073-1; AT21_075-1; AT21_089-1; AT21_093-1; AT21_097-1; AT21_098-1; AT21_104-1; AT21_106-1; AT21_107-1; AT21_108-1; AT21_109-1; AT21_110-1; AT21_111-1; AT21_112-1; AT21_113-1; AT21_114-1; AT21_117-1; AT21_119-1; AT21_122-1; AT21_125-1; Barents Sea; Bottle number; Calculated; CATS; CATS - The Changing Arctic Transpolar System; Conductivity; CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Fluorescence, chlorophyll; Fluorometer, WET Labs ECO AFL/FL; Kara Sea; Laptev Sea; Latitude of event; Longitude of event; Nitrate; Nitrite; nutrients; Oxygen, dissolved; pH; Phosphate; physical oceanography; Potentiometric titration, Metrohm 916 TiTouch; Pressure, water; Salinity; Sample code/label; Segmented flow analyzer, Seal Analytical; shelf-basin transects; Silicate; Spectrophotometer Shimadzu UV-1800; St. Anna Trough; Station label; Temperature, water; Titration, Winkler
    Type: Dataset
    Format: text/tab-separated-values, 21531 data points
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  • 8
    Publication Date: 2024-01-24
    Description: Underway-CTD (UCTD) data were collected during an August-September 2021 expedition to the Arctic Ocean aboard the RV Akademik Tryoshnikov. The underway CTD manufactured by Ocean Science is a self-contained free-falling probe measuring temperature, conductivity, depth while the ship is transiting. The UCTD was operated mostly in yoyo-mode during selected transects on the shelf of the Kara and Laptev Seas and between the shelf and the basin across the continental slope of the Eurasian Basin while the ship was transiting with 4 - 10 knots. The UCTD probe records the start time of the measurements and stores 16 samples each second internally. The exact location of each profile was subsequently found based on the time stamp from the cruise track. The unpumped conductivity sensor has a slower response time than the temperature sensor, which makes the computation of salinity from conductivity and temperature potentially spiky, especially in the pycnocline or in frontal regions. We followed the recommendation of the manufacturer to calculate salinity with Seabird processing software. The salinity is given as Practical Salinity (PSU). The raw data profiles are provided as well and can be reprocessed if desired. In shallower waters (〈300 m), the water column was profiled all the way to the seafloor, while in deeper waters, only the upper 300-600 m were sampled. The UCTD was calibrated against a Seabird 9+ CTD during the cruise. The upper 5 m of the data were discarded due to the influence of the ship. The icebreaker Akademik Tyoshnikov has a deep draft. Mixing of the water column caused by the ship can reach depths of up to about 10 m, depending on the weather conditions and the ship's speed. The data are provided by the Arctic Century Expedition, a joint initiative led by the Swiss Polar Institute (SPI), the Antarctic and Arctic Research Institute (AARI) and GEOMAR Helmholtz Centre for Ocean Research Kiel (GEOMAR) and funded by the Swiss Polar Foundation, AARI, Minobrnauki (CATS RFMEFI61619X0108) and BMBF (CATS 03F0831)
    Keywords: Akademik Tryoshnikov; ArcticCentury; Arctic Century Expedition; Arctic Ocean; AT21; AT21_015-A; AT21_016-A; AT21_016-B; AT21_017-A; AT21_017-B; AT21_020-A; AT21_025-A; AT21_025-B; AT21_025-C; AT21_025-D; AT21_026-A; AT21_027-A; AT21_028-A; AT21_029-A; AT21_030-A; AT21_037-A; AT21_042; AT21_044; AT21_046; AT21_048; AT21_052; AT21_054; AT21_070-A; AT21_070-B; AT21_070-C; AT21_070-D; AT21_070-E; AT21_070-F; AT21_079-C; AT21_079-D; AT21_079-E; AT21_079-F; AT21_079-G; AT21_079-H; AT21_079-I; AT21_079-J; AT21_079-K; AT21_079-L; AT21_079-M; AT21_079-N; AT21_079-O; AT21_079-P; AT21_079-Q; AT21_079-R; AT21_079-S; AT21_079-T; AT21_079-U; AT21_081; AT21_082; AT21_083; AT21_084; AT21_085; AT21_086; AT21_087; AT21_088; AT21_090; AT21_091; AT21_094; AT21_095; AT21_099; AT21_100; AT21_101; AT21_102; AT21_105; AT21_115; AT21_118; AT21_120; AT21_121; AT21_123; AT21_124; Barents Sea; CATS; CATS - The Changing Arctic Transpolar System; Conductivity; CTD, underway; CTD-UW; Date/Time of event; DEPTH, water; Elevation of event; Event label; Kara Sea; Laptev Sea; Latitude of event; Longitude of event; Pressure, water; Salinity; Station label; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 103960 data points
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  • 9
    Publication Date: 2024-02-27
    Description: The data set includes the light absorption coefficient of colored dissolved organic matter (CDOM) from 200 nm to 700 nm wavelength and dissolved organic carbon (DOC) together with physical oceanographic observations (temperature and salinity) from the Laptev Sea and East Siberian Sea. Sampling was carried out September and October 2019. During the ship-based expedition, we operated a CTD profiler (conductivity temperature-depth; Seabird 911+) to sample the basic hydrographic parameters. The CTD is operated on a carousel water sampler (SBE 32), which can take water samples at the selected depths. The dataset is part of a multi-year study (different seasons over a period of 9 years: 2010-2019) of the dissolved organic matter (CDOM), which includes observations in marine waters from the coastal zone to the shelf edge of the Laptev Sea and East Siberian Sea, the river Lena and ice and water samples from the land-fast in the south-eastern Laptev Sea.
    Keywords: Absorption coefficient, colored dissolved organic matter at given wavelength; Area/locality; Bering Strait; Carbon, organic, dissolved; CATS; CATS - The Changing Arctic Transpolar System; CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; DATE/TIME; Depth, bathymetric; DEPTH, water; Dissolved Organic Matter; East Siberian Sea; Event label; High Temperature Catalytic Oxidation (Shimadzu TOC-VCPN); Landfast ice; Laptev Sea; Laptev Sea System; LATITUDE; LONGITUDE; LSS; PM19_113; PM19_117; PM19_119; PM19_120; PM19_122; PM19_124; PM19_129; PM19_133; PM19_135; PM19_137; PM19_139; PM19_140; PM19_160; PM19_161; PM19_162; PM19_163; PM19_164; PM19_165; PM19_166; PM19_167; PM19_168; PM19_169; PM19_170; PM19_171; PM19_172; PM19_173; PM19_174; PM19_175; PM19_176; PM19_177; PM19_178; PM19_179; PM19_180; PM19_181; PM19_184; PM19_193; PM19_194; PM19_195; PM19_196; PM19_197; PM19_198; PM19_199; Professor Multanovskiy; River Lena; Salinity; Siberian Shelf Seas; Spectrophotometer, dual beam (Specord200, Jena Analytik); Station label; Temperature, water; Transarktika-2019_Leg4
    Type: Dataset
    Format: text/tab-separated-values, 99507 data points
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