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  • Data  (22,026)
  • 2020-2022
  • 2020-2020
  • 2015-2019  (22,026)
  • 1945-1949
  • 2018  (9,608)
  • 2016  (12,418)
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  • 2020-2022
  • 2020-2020
  • 2015-2019  (22,026)
  • 1945-1949
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  • 1
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Description: The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled balloons (TOTEX 600 g, 800 g) were used to carry Vaisala RS92-SGPW radiosondes. Whenever possible, the launches were performed about 10 UTC. Condensed measurements (TEMP Format FM-35) were transferred without delay into the Global Telecommunication System GTS were they contribute for the world wide weather forecasts. The profile data were taken every 5-10 seconds which result in a vertical profile resolution of about 25-50 meter. The profiles start at the helideck 10 m above sea level and terminate at the burst level of the balloons, normally at heights between 25 and 37 km.
    Keywords: AWI_Meteo; Meteorological Long-Term Observations @ AWI
    Type: Dataset
    Format: application/zip, 136 datasets
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  • 2
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    PANGAEA
    In:  Supplement to: Kremer, Anne; Stein, Ruediger; Fahl, Kirsten; Ji, Z; Yang, Z; Wiers, Steffen; Matthiessen, Jens; Forwick, Matthias; Löwemark, Ludvig; O'Regan, Matthew; Chen, Jiaming; Snowball, Ian (2018): Changes in sea ice cover and ice sheet extent at the Yermak Plateau during the last 160 ka - Reconstructions from biomarker records. Quaternary Science Reviews, 182, 93-108, https://doi.org/10.1016/j.quascirev.2017.12.016
    Publication Date: 2023-03-16
    Description: The Yermak Plateau is located north of Svalbard at the entrance to the Arctic Ocean, i.e. in an area highly sensitive to climate change. A multi proxy approach was carried out on Core PS92/039-2 to study glacial-interglacial environmental changes at the northern Barents Sea margin during the last 160 ka. The main emphasis was on the reconstruction of sea ice cover, based on the sea ice proxy IP25 and the related phytoplankton - sea ice index PIP25. Sea ice was present most of the time but showed significant temporal variability decisively affected by movements of the Svalbard Barents Sea Ice Sheet. For the first time, we prove the occurrence of seasonal sea ice at the eastern Yermak Plateau during glacial intervals, probably steered by a major northward advance of the ice sheet and the formation of a coastal polynya in front of it. Maximum accumulation of terrigenous organic carbon, IP25 and the phytoplankton biomarkers (brassicasterol, dinosterol, HBI III) can be correlated to distinct deglaciation events. More severe, but variable sea ice cover prevailed at the Yermak Plateau during interglacials. The general proximity to the sea ice margin is further indicated by biomarker (GDGT) - based sea surface temperatures below 2.5 °C.
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_Paleo; KAL; Kasten corer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS92; PS92/039-2
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 3
    Publication Date: 2023-03-16
    Description: Past sea ice conditions and open water phytoplankton production were reconstructed from a sediment core taken in Disko Bugt, West Greenland, using the sea ice biomarker IP~25~ and other specific phytoplankton biomarker (i.e., brassicasterol, dinosterol, HBI III) records. Our biomarker record indicates that Disko Bugt experienced a gradual expansion of seasonal sea ice during the last 2.2 kyr. Maximum sea ice extent was reached during the Little Ice Age around 0.2 kyr BP. Superimposed on this longer term trend, we find short-term oscillations in open water primary production and terrigenous input, which may be related to the Atlantic Multidecadal Oscillation and solar activity changes as potential climatic trigger mechanisms. A direct sample-to-sample multiproxy comparison of our new biomarker record with microfossil (i.e., benthic foraminifera, dinocysts, and diatoms) and other geochemical records (i.e., alkenone biomarkers) indicates that different proxies are influenced by the complex environmental system with pronounced seasonal changes and strong oceanographic gradients, e.g., freshwater inflow from the Greenland Ice Sheet. Differences in sea ice reconstructions may indicate that the IP~25~ record reflects only the relatively short sea ice season (spring), whereas other microfossil reconstructions may reflect a longer (spring–autumn) interval.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Description: Using a microprofiler and electrochemical oxygen sensors after Revsbech (1989) in situ oxygen profiles measurements were conducted with a spatial resolution if 100 µm and a temporal resolution of 30 seconds at three stations in Potter Cove in austral summer 2015.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Braeckman, Ulrike; Janssen, Felix; Lavik, Gaute; Elvert, Marcus; Marchant, Hannah K; Buckner, Caroline; Bienhold, Christina; Wenzhöfer, Frank (2018): Carbon and nitrogen turnover in the Arctic deep sea: in situ benthic community response to diatom and coccolithophorid phytodetritus. Biogeosciences, 15(21), 6537-6557, https://doi.org/10.5194/bg-15-6537-2018
    Publication Date: 2023-03-16
    Description: This is a dataset from an in situ experiment at station S2 from the LTER monitoring site HAUSGARTEN, performed in June-July 2013 during Maria S Merian expedition MSM29. The in situ responses of Arctic deep-sea benthos to input of phytodetritus of a diatom (Thalassiosira sp.) as opposed to a coccolithophorid (Emiliania huxleyi) were investigated in incubation chambers of benthic landers. Using 13C and 15N labelled phytodetritus harvested from cultures of these species, we traced the fate of the respective phytodetritus into different parts of the food web (respiration, assimilation by bacteria and infauna 〉250 µm), in a short (4d) and long (14d) term experiment. The benthic landers were lowered to the sea floor, where they enclosed ~ 20cm of sediment and ~10 cm of overlying water. During respectively 4d and 14d, the temperature and concentrations of O2, DIC, 13C-DIC, NHx, NOx, 15N-NH4, 15N-NOx were measured. Upon recovery of the landers, the sediment was retrieved and subsampled in vertical horizons to measure pigment, TOC and TN, 13C-POC and 15N-PN concentrations, pore water concentrations of DIC, 13C-DIC, NHx, NOx, 15N-NH4 and 15N-NOx and the assimilation of 13C in bacterial fatty acids (iC15:0 and aiC15:0) and in fauna 〉 250 µm
    Keywords: Hausgarten; Long-term Investigation at AWI-Hausgarten off Svalbard
    Type: Dataset
    Format: application/zip, 10 datasets
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  • 6
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    PANGAEA
    In:  Supplement to: Izett, Robert W; Manning, Cara C M; Hamme, Roberta C; Tortell, Philippe Daniel (2018): Refined Estimates of Net Community Production in the Subarctic Northeast Pacific Derived From ΔO2/Ar Measurements With N2O-Based Corrections for Vertical Mixing. Global Biogeochemical Cycles, 32(3), 326-350, https://doi.org/10.1002/2017GB005792
    Publication Date: 2023-03-16
    Description: We present the first field application of a N2O-based approach to correct for vertical mixing in the estimation of net community production (NCP) from mixed layer O2 measurements. Using new ship-based observations of N2O and biological oxygen saturation anomalies (DeltaO2/Ar) from the Subarctic Northeast Pacific, we provide refined mixed layer NCP estimates across contrasting hydrographic regimes and a comprehensive assessment of the methodological considerations and limitations of the approach. Increased vertical mixing coefficients at the base of the mixed layer, derived using N2O measurements, corresponded with periods of heightened wind speed and coastal upwelling. Corrections were most significant in coastal regions where the vertical supply of low-O2 water can otherwise falsely imply net heterotrophy from negative DeltaO2/Ar measurements. After correcting for the mixing flux, all coastal stations showed autotrophic signatures, with maximum NCP exceeding 100 mmol O2 m-2 day-1 in the spring and summer. Vertical fluxes were lower in off-shelf waters, but often contributed more than 50 % to corrected NCP. At some oceanic stations, however, the co-occurrence of N2O minima and O2 maxima resulted in biased (over-estimated) N2O corrections. Evaluating vertical fluxes in these regions remains a challenge for ship-based studies. Nonetheless, our refined NCP estimates show better coherence with surface chlorophyll, temperature, and mixed layer depth than uncorrected values. Potential mixed layer N2O production introduces some uncertainty in the approach, but errors are likely to be small. Ultimately, this work provides rationale for the adoption of the N2O correction to refine NCP estimates, particularly in coastal waters. Data in this submission include the ancillary components required to replicate all calculations, and conclusions made in the main manuscript.
    Type: Dataset
    Format: application/zip, 20 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Kruse, Stefan; Epp, Laura Saskia; Wieczorek, Mareike; Pestryakova, Luidmila A; Stoof-Leichsenring, Kathleen Rosmarie; Herzschuh, Ulrike (2018): High gene flow and complex treeline dynamics of Larix Mill. stands on the Taymyr Peninsula (north-central Siberia) revealed by nuclear microsatellites. Tree Genetics & Genomes, 14(2), https://doi.org/10.1007/s11295-018-1235-3
    Publication Date: 2023-03-16
    Description: Arctic treelines are facing a strong temperature increase as a result of recent global warming, causing possible changes in forest extent, which will alter vegetation-climate feedbacks. However, the mode and strength of the response is rather unclear, as potential changes are happening in areas that are very remote and difficult to access, and empirical data are still largely lacking. Here, we assessed the current population structure and genetic differentiation of Larix Mill. tree stands within the northernmost latitudinal treeline reaching ~72° N in the southern lowlands of the Taymyr Peninsula (~100° E). We sampled 743 individuals belonging to different height classes (seedlings, saplings, trees) at eleven locations along a gradient from 'single tree' tundra over 'forest line' to 'dense forest' stands and conducted investigations applying eight highly polymorphic nuclear microsatellites. Results suggest a high diversity within subpopulations (HE=0.826-0.893), coupled, however, with heterozygote deficits in all subpopulations, but pronounced in 'forest line' stands. Overall, genetic differentiation of subpopulations is low (FST=0.005), indicating a region-wide high gene flow, although 'forest line' stands harbour few rare and private alleles, likely indicating greater local reproduction. 'Single tree' stands, located beyond the northern forest line, are currently not involved in treeline expansion, but show signs of a long-term refuge, namely asexual reproduction and change of growth-form from erect to creeping growth, possibly having persisted for thousands of years. The lack of differentiation between the subpopulations points to a sufficiently high dispersal potential, and thus a rapid northward migration of the Siberian arctic treeline under recent global warming seems potentially unconstrained, but observations show it to be unexpectedly slow.
    Keywords: AWI_Envi; Polar Terrestrial Environmental Systems @ AWI
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
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    PANGAEA
    In:  Supplement to: Beamish, Alison Leslie; Coops, Nicholas; Chabrillat, Sabine; Heim, Birgit (2017): A phenological approach to spectral differentiation of low-arctic tundra vegetation communities, North Slope, Alaska. Remote Sensing, 9(12), 1200, https://doi.org/10.3390/rs9111200
    Publication Date: 2023-03-16
    Description: Ground-based spectroscopy measurements acquired systematically within the Toolik Vegetation Grid in the 2015 and 2016 growing seasons and within the Imnavait Vegetation Grid in the 2016 growing season. Data were collected in 68 distinct 1 x 1 m long-term monitoring plots representing five distinct vegetation communities. Spectral measurements were acquired two times throughout the season in 2015 representing peak and late season and three times in 2016 representing early, peak and late season. Data were acquired using a GER 1500 field spectrometer (350-1050 nm; 512 bands, spectral resolution 3 nm, spectral sampling 1.5 nm, and 8! field of view). Spectra were collected under clear weather conditions at the highest solar zenith angle between 10:00 and 14:00 local time. Data were collected at nadir approximately 1 m off the ground resulting in a Ground Instantaneous Field of View (GIFOV) of approximately 15 cm in diameter. Nine point measurements of upwelling radiance (Lup) were collected in 1 x 1 m plots representative of the five vegetation communities and averaged to characterize the spectral variability and to reduce noise. Downwelling radiance (Ldown) was measured as the reflectance from a white Spectralon© plate. Surface reflectance (R) was processed as Lup/Ldown x 100 (0-100%). Reflectance spectra were preprocessed with a Savitzky-Golay smoothing filter (n = 11) and subset to 400-985 nm to remove sensor noise at the edges of the radiometer detector.
    Keywords: AWI_Envi; MULT; Multiple investigations; Polar Terrestrial Environmental Systems @ AWI; ToolikL_plot; Toolik Lake, Alaska
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 9
    Publication Date: 2023-03-16
    Description: Our data, as part of the OISO (Ocean Indien Service d'Observation) campaign, contributes to a better understanding of the physical and biological factors controlling N2 fixation in the Southern Indian Ocean and the French Southern and Antarctic lands during Austral summer January and February 2017. We measured N2 and C fixation as well as NH4+ and NO3- assimilation in 3-6 replicates per station. Additionally, we measured diagnostic pigment concentrations to evaluate phtosynthetic community composition. For pigment analysis 4L water was filtered through 25mm Whatman GF/F filters (pressure drop 〈10kPa). Samples were stored at -80°C until analysis. Pigments were analysed using High Performance Liquid Chromatography (HPLC). Pigment concentration were calculated according to Kilias et al (2013, doi:10.1111/jpy.12109). N2 fixation experiments were carried out in three to six replicates for each station. Incubations were done in pre-acid washed polycarbonate bottles on deck with ambient light conditions. All polycarbonate incubation bottles were rinsed with deionized water, and seawater prior to incubation. We used the combination of the bubble approach (Montoya et al., 1996) and the dissolution method (Mohr et al., 2010, doi:10.1371/journal.pone.0012583) proposed by Klawonn et al. (2015, doi:10.3389/fmicb.2015.00769). Bottles were filled up to capacity to avoid air contamination. Incubations were initialized by adding a 10 ml 15-15N gas bubble. Bottles were gently rocked for 15 minutes. Finally, the remaining bubble was removed to avoid equilibration between gas and aqueous phase. after 24 hours a water subsample was taken to a 12 ml exetainer and preserved with 100 µl HgCl2 solution for later determination of exact 15N-15N concentration. Natural 15N2 was determined using Membrane Inlet Mass Spectrometry (MIMS; GAM200, IPI) for each station. Analysis of 15N2 incorporated was carried out by the Isotopic Laboratory at the UC Davis, California campus. We used stable isotope tracers (15N) to measure dissolved inorganic nitrogen (DIN) assimilation rates. Experiments were initiated by adding a known concentration of 0.05 of K15NO3 and 15NH4Cl for oligotrophic waters of the IO and 0.625 µmol L-1 for HNLC regions in the ACC and PF (Knap et al., 1994, Waite et al., 2007, doi:10.1016/j.dsr2.2006.12.010) to one litre polycarbonate bottles. For C assimilation experiments, we added 20 µmol L-1 of NaH13CO3 to one of each of N2 fixation, NH4+ and NO3- assimilation experiment bottles. For incubation, we followed the same procedure as for N2 fixation experiments. Findings reveal that N2 fixation occurs throughout the whole sampling area up to 55°S latitude. In addition, variations of N2 fiaxation rates between replicates were relatively high indicating a great heterogeneity of the French Southern and Antarctic waters. References: Montoya 1996: Montoya, Joseph P., et al. "A Simple, High-Precision, High-Sensitivity Tracer Assay for N (inf2) Fixation." Applied and environmental microbiology 62.3 (1996): 986-993. Knap et al 1994: Knap, A., Michaels, A., Close, A., Ducklow, H. & Dickson, A. 1994. Protocols for the Joint Global Ocean Flux Study (JGOFS) Core Measurements, JGOFS, Reprint of the IOC Manuals and Guides No. 29. UNESCO, 19, 1.
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: van der Jagt, Helga; Friese, Carmen A; Stuut, Jan-Berend W; Fischer, Gerhard; Iversen, Morten Hvitfeldt (2018): The ballasting effect of Saharan dust deposition on aggregate dynamics and carbon export: Aggregation, settling, and scavenging potential of marine snow. Limnology and Oceanography, 63(3), 1386-1394, https://doi.org/10.1002/lno.10779
    Publication Date: 2023-03-16
    Description: Lithogenic material such as Saharan dust can be incorporated into organic aggregates and act as ballast, potentially enhancing the marine carbon export via increased sinking velocities of aggregates. We studied the ballasting effects of Saharan dust on the aggregate dynamics in the upwelling region off Cape Blanc (Mauritania). Aggregate formation from a natural plankton community exposed to Saharan dust deposition resulted in higher abundance of aggregates with higher sinking velocities compared to aggregate formation with low dust. This higher aggregate abundance and sinking velocities potentially increased the carbon export 10-fold when the aggregates were ballasted by Saharan dust. After aggregate formation in the surface waters, subsequent sinking through suspended Saharan dust minerals had no influence on aggregate sizes, abundance, and sinking velocities. We found that aggregates formed in the surface ocean off Mauritania were already heavily ballasted with lithogenic material and could therefore not scavenge any additional minerals during their descent. This suggests that carbon export to the deep ocean in regions with high dust deposition is strongly controlled by dust input to the surface ocean while suspended dust particles in deeper water layers do not significantly interact with sinking aggregates.
    Keywords: Center for Marine Environmental Sciences; MARUM; SeaPump; Seasonal and regional food web interactions with the biological pump
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 11
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    PANGAEA
    In:  Supplement to: Beamish, Alison Leslie; Coops, Nicholas; Hermosilla, T; Chabrillat, Sabine; Heim, Birgit (2018): Monitoring pigment-driven vegetation changes in a low-Arctic tundra ecosystem using digital cameras. Ecosphere, 9(2), e02123, https://doi.org/10.1002/ecs2.2123
    Publication Date: 2023-03-16
    Description: Ground-based spectroscopy measurements acquired systematically within the Toolik Vegetation Grid in the 2016 growing season. All data were collected in a subset of 1 x 1 m long-term monitoring plots representing three distinct vegetation communities three times representing early, peak and late season. Spectral data were acquired using a GER 1500 field spectrometer (350-1050 nm; 512 bands, spectral resolution 3 nm, spectral sampling 1.5 nm, and 8! field of view). Spectra were collected under clear weather conditions at the highest solar zenith angle between 10:00 and 14:00 local time. Data were collected at nadir approximately 1 m off the ground resulting in a Ground Instantaneous Field of View (GIFOV) of approximately 15 cm in diameter. Nine point measurements of upwelling radiance (Lup) were collected in each plot and averaged to characterize the spectral variability and to reduce noise. Downwelling radiance (Ldown) was measured as the reflectance from a white Spectralon© plate. Surface reflectance (R) was processed as Lup/Ldown x 100 (0-100%). Reflectance spectra were preprocessed with a Savitzky-Golay smoothing filter (n = 11) and subset to 400-985 nm to remove sensor noise at the edges of the radiometer detector. Digital camera data were acquired using a consumer-grade camera (Panasonic DM3 LMX, Japan) approximately 1 m off the ground with a white frame for registration of off nadir images. For detailed definitions of the RGB indices see metadata.docx. Leaves and stems of the dominant vascular species in a subset of the sampled plots were collected at early, peak, and late season for chlorophyll and carotenoid analysis.Samples were placed in porous tea bags and preserved in a silica gel desiccant in an opaque container for up to 3 months until pigment extraction (Esteban et al. 2009, doi:10.1007/s11120-009-9468-5). Each sample was homogenized by grinding with a mortar and pestle. Approximately 1.00 mg (+/- 0.05 mg) of homogenized sample was placed into a vial with 2 ml of dimethylformamide (DMF). Vials were then wrapped in aluminum foil to eliminate any degradation of pigments due to UV light and stored in a fridge (4C) for 24 hrs. Samples were measured into a cuvette prior to spectrophotometric analysis. Bulk pigments concentrations were then estimated using a spectrophotometer measuring absorption at 646.8, 663.8 and 480 nm (Porra et al. 1989, doi:10.1016/S0005-2728(89)80347-0) . Absorbance (A) values at specific wavelengths were transformed into µg/mg concentrations of chlorophyll a, Chla, chlorophyll b, Chlb, total chlorophyll, Chl, carotenoids, Car (for equations see metadata.docx). Pigment concentration was calculated as the average concentration of the dominant species in each plot. mean_"pigment" represents the mean of all biomass from each vegetation community and sd_"pigment" represents the standard deviation of each vegetation community.
    Keywords: AWI_Envi; MULT; Multiple investigations; Polar Terrestrial Environmental Systems @ AWI; ToolikL_plot; Toolik Lake, Alaska
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 12
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    PANGAEA
    In:  Supplement to: Park, Eunmi; Hefter, Jens; Fischer, Gerhard; Mollenhauer, Gesine (2018): TEX86 in sinking particles in three eastern Atlantic upwelling regimes. Organic Geochemistry, 124, 151-163, https://doi.org/10.1016/j.orggeochem.2018.07.015
    Publication Date: 2023-03-16
    Description: Seasonal variations in fluxes of isoprenoid glycerol dialkyl glycerol tetraethers (GDGTs) and the estimated temperatures based on TEX86 are examined in sinking particles collected using moored sediment traps in the eastern Atlantic upwelling regions. In the equatorial Guinea Basin, GDGT fluxes show a correlation with opal fluxes, implying that GDGTs are mainly transported via aggregation with diatoms. The flux-weighted TEXH86 temperatures derived from particles collected both at 853 m and 3,921 m depth correspond to the water temperature (24.1 °C) of ca. 50 m depth, where nitrate concentration starts to increase, potentially as a consequence of nitrification by Thaumarchaeota. This suggests that nutrient concentrations may affect the depth habitat of Thaumarchaeota, and it determines at which water depth the TEXH86 temperature is recorded. In the coastal upwelling off Namibia, TEXH86 temperatures are similar to satellite-derived sea surface temperature (SST) during the warm season, but the record derived from the trap is delayed relative to the SST by approximately 26 days. Warm biases, however, occur during the cold season, similar to what has previously been observed in the filamentous upwelling region off Cape Blanc. In both coastal upwelling regions, oxygen minimum zones (OMZs) are a common feature, and higher TEX86 values have been found within the OMZs in the water column off Cape Blanc and elsewhere. Thus, contributions from GDGTs produced in OMZs might explain the warmer temperature estimates during the cold season in both regions. We thus conclude that in the eastern Atlantic upwelling system, TEXH86 temperature estimates are influenced by non-thermal factors such as nutrient depth distributions and GDGTs produced in the OMZ. In paleoenvironmental records of TEX86, non-thermal signals have to be considered on regional scales.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 13
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    PANGAEA
    In:  Supplement to: Pauli, Nora-Charlotte; Paiva, Filipa; Briski, Elizabeta (2018): Are Ponto-Caspian species able to cross salinity barriers? A case study of the gammarid Pontogammarus maeoticus. Ecology and Evolution, 8(19), 9817-9826, https://doi.org/10.1002/ece3.4461
    Publication Date: 2023-03-16
    Description: Recently, Ponto-Caspian species (i.e. area of Azov, Black and Caspian Seas) have invaded brackish and freshwater habitats of the North and Baltic Seas and the Laurentian Great Lakes in much higher numbers than expected based on shipping frequency and environmental conditions among these regions. Therefore, it has been hypothesized that Ponto-Caspian species may have inherent advantages over other species in colonizing new habitats, or that they are of freshwater origin. To test these hypotheses, we conducted artificial selection experiment on Ponto-Caspian amphipod Pontogammarus maeoticus collected from 10 PSU to evaluate adaptation capacity of this species to different salinities. Our results indicated that selection to lower salinity than that of population's ambient salinity is possible. Though, generation time in lower salinity conditions took slightly longer. On the contrary, selection to higher salinity was unsuccessful. Taking into account the results from this and previous studies and the geological history of the Ponto-Caspian region, we suggest that majority of the Ponto-Caspian relict fauna might be of freshwater origin and lack necessary genetic background for adaptation to fully marine conditions. Further selection studies using more species and populations, as well as molecular techniques, should be conducted to confirm this hypothesis on a broader scale. Consequently, if Ponto-Caspian relict species are of freshwater origin, the perception that they are better colonizers than species from other regions might be inclined by the fact that areas with biggest introduction frequency of nonindigenous species (i.e., shipping ports) are environmentally variable habitats which often include freshwater conditions.
    Keywords: AWI_BioOce; Biological Oceanography @ AWI
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    Format: application/zip, 2 datasets
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  • 14
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    PANGAEA
    In:  Supplement to: Hörner, Tanja; Stein, Ruediger; Fahl, Kirsten (2018): Paleo-sea ice distribution and polynya variability on the Kara sea shelf during the last 12 ka. arktos - The Journal of Arctic Geosciences, https://doi.org/10.1007/s41063-018-0040-4
    Publication Date: 2023-03-16
    Description: The Kara Sea is an important area for paleo-climatic research since sea ice and brine formation take place on its shelf-two processes inducing supra-regional climatic implications and thereby connecting regional environmental variability with global climatic conditions. To gain information about past sea ice coverage and variations, three sediment cores distributed in the southern and central parts of the marginal Sea were investigated. By applying the sea ice biomarker IP25 and the PIP25 index [phytoplankton biomarker (dinosterol)-IP25 index] post-glacial sea ice variability could be detected in the central Kara Sea (Core BP00-36/4), with most intense sea ice cover between 12.4 and 11.8 ka coinciding with the Younger Dryas (12.9-11.6 ka), and reduced sea ice cover between 10 and 8 ka during the Holocene Thermal Maximum. During the last ~7 ka, increasing sea ice indicators might indicate a Holocene cooling trend, probably induced by declining summer insolation. Furthermore, temporal changes in the fast ice?polynya distribution in the southern Kara Sea were detected: expanding fast ice during the late Holocene and a cyclic short-term Holocene climate variability documented by abrupt changes in the sea ice coverage at the BP00-07/7 core site. Core BP99-04/7 from the Yenisei estuary recorded consistently seasonal sea ice cover since ~9.3 ka, apart from five short phases of fast ice expansion to the core site. The strong influence of river run-off as well as estuary processes might prevent the detection of (short-term) climatic signals at this study site.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
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    Format: application/zip, 3 datasets
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  • 15
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    PANGAEA
    In:  Supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791, https://doi.org/10.1038/srep25791
    Publication Date: 2023-03-13
    Description: Extra-tropical circulation systems impede poleward moisture advection by the Indian Summer Monsoon. In this context, the Himalayan range is believed to insulate the south Asian circulation from extra-tropical influences and to delineate the northern extent of the Indian Summer Monsoon in central Asia. Paleoclimatic evidence, however, suggests increased moisture availability in the Early Holocene north of the Himalayan range which is attributed to an intensification of the Indian Summer Monsoon. Nevertheless, mechanisms leading to a surpassing of the Himalayan range and the northern maximum extent of summer monsoonal influence remain unknown. Here we show that the Kunlun barrier on the northern Tibetan Plateau [~36°N] delimits Indian Summer Monsoon precipitation during the Holocene. The presence of the barrier relocates the insulation effect 1,000 km further north, allowing a continental low intensity branch of the Indian Summer Monsoon which is persistent throughout the Holocene. Precipitation intensities at its northern extent seem to be driven by differentiated solar heating of the Northern Hemisphere indicating dependency on energy-gradients rather than absolute radiation intensities. The identified spatial constraints of monsoonal precipitation will facilitate the prediction of future monsoonal precipitation patterns in Central Asia under varying climatic conditions.
    Keywords: AWI_PerDyn; Permafrost Research (Periglacial Dynamics) @ AWI
    Type: Dataset
    Format: application/zip, 17 datasets
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  • 16
    Publication Date: 2023-03-14
    Keywords: Acidity; Alkalinity, total; Ammonium; AWI_PerDyn; AWI_POK-01; AWI Arctic Land Expedition; Bottom water temperature; Conductivity, electrolytic; DATE/TIME; Depth, bottom/max; DEPTH, water; Hardness description; Kytalyk-Pokhodsk_2012, Kolyma2012; Monitoring station; MONS; Nitrate; Oxygen; Permafrost Research (Periglacial Dynamics) @ AWI; pH; Phosphate; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Siberia, Russia; Temperature, air; Temperature, water; Thaw depth of active layer
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 17
    Publication Date: 2023-03-14
    Keywords: AWI_PerDyn; AWI_Pi01; AWI_Pi02; AWI_Pi03; AWI_Pi04; AWI_Pi05; AWI_Pi06; AWI_Pi07; AWI_Pi08; AWI_Pi09; AWI_Pi10; AWI_Pi11; AWI_Pi12; AWI_Pi13; AWI_Pi14; AWI_PiL; AWI Arctic Land Expedition; DEPTH, soil; Depth, soil, maximum; Depth, soil, minimum; East Siberia; Event label; islet1; islet2.center; islet2.wall; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2012_Kytalyk_Kolyma; Sampling/measurement on land; Siberia, Russia; Soil horizon; Soil type
    Type: Dataset
    Format: text/tab-separated-values, 195 data points
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  • 18
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20140822; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 22440 data points
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  • 19
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20150828; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 46315 data points
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  • 20
    Publication Date: 2023-03-14
    Keywords: BIOACID; BIOACID 2 PNG2013; Biological Impacts of Ocean Acidification; DATE/TIME; DIVER; Environment; LATITUDE; Layer description; Location; LONGITUDE; M.V. Chertan; Number; Papua_New_Guinea_CO2_vent; pH; Sample code/label; Sample ID; Sampling by diver
    Type: Dataset
    Format: text/tab-separated-values, 112 data points
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  • 21
    Publication Date: 2023-03-14
    Keywords: Change; Darlington; DATE/TIME; EXP; Experiment; Oxygen saturation; pH; pH change; Replicate; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 168 data points
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  • 22
    Publication Date: 2023-03-14
    Keywords: Darlington; DATE/TIME; DEPTH, water; Event label; EXP; Experiment; Fortescue_Bay; Habitat; LATITUDE; LONGITUDE; Oxygen; pH; ph electrode; pHTempion; Replicate; Salinity; SeaPHOX; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 9497 data points
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  • 23
    Publication Date: 2023-03-14
    Description: Ocean acidification causes an accumulation of CO2 in marine organisms and leads to shifts in acid-base parameters. Acid-base regulation in gill breathers involves a net increase of internal bicarbonate levels through transmembrane ion exchange with the surrounding water. Successful maintenance of body fluid pH depends on the functional capacity of ion-exchange mechanisms and associated energy budget. For a detailed understanding of the dependence of acid-base regulation on water parameters, we investigated the physiological responses of the shore crab Carcinus maenas to 4 weeks of ocean acidification [OA, P(CO2)w = 1800 µatm], at variable water bicarbonate levels, paralleled by changes in water pH. Cardiovascular performance was determined together with extra-(pHe) and intracellular pH (pHi), oxygen consumption, haemolymph CO2 parameters, and ion composition. High water P(CO2) caused haemolymph P(CO2) to rise, but pHe and pHi remained constant due to increased haemolymph and cellular [HCO3-]. This process was effective even under reduced seawater pH and bicarbonate concentrations. While extracellular cation concentrations increased throughout, anion levels remained constant or decreased. Despite similar levels of haemolymph pH and ion concentrations under OA, metabolic rates, and haemolymph flow were significantly depressed by 40 and 30%, respectively, when OA was combined with reduced seawater [HCO3-] and pH. Our findings suggest an influence of water bicarbonate levels on metabolic rates as well as on correlations between blood flow and pHe. This previously unknown phenomenon should direct attention to pathways of acid-base regulation and their potential feedback on whole-animal energy demand, in relation with changing seawater carbonate parameters.
    Keywords: Bicarbonate; Eggs, hatched; EXP; Experiment; Incubation duration; pH; Pressure, air; Salinity; Spiekeroog_Island; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 288 data points
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  • 24
    Publication Date: 2023-03-13
    Keywords: AWI_PerDyn; AWI Arctic Land Expedition; Calculated; China2011,China2012/1,China2012/2,China2012/3; Cluster membership; CN-Land_2012; Date/Time of event; DEPTH, sediment/rock; Event label; HAND; HH-11154; HH-11163; HH-11192; HH-11199; HH-11211; HH-11278; HH-11285; HH-11286; HH-11287; HH-11316; HH-2012-08-20-001; HH-2012-08-20-003; HH-2012-08-20-004; HH-2012-08-20-005; HH-2012-08-20-006; HH-2012-08-20-007; HH-2012-08-20-008; HH-2012-08-20-010; HH-2012-08-20-011; HH-2012-08-20-012; HH-2012-08-20-013; HH-2012-08-20-014; HH-2012-08-20-016; HH-2012-08-20-017a; HH-2012-08-20-017b; HH-2012-08-20-018; HH-2012-08-20-019; HH-2012-08-20-020; HH-2012-08-20-021; HH-2012-08-20-022; HH-2012-08-20-023a; HH-2012-08-20-023b; HH-2012-08-20-024; HH-2012-08-20-025; HH-2012-08-20-029; HH-2012-08-21-001; HH-2012-08-21-002; HH-2012-08-21-004; HH-2012-08-21-006; HH-2012-08-21-007; HH-2012-08-21-008; HH-2012-08-21-009; HH-2012-08-23-001; HH-2012-08-23-004; HH-2012-08-23-006; HH-2012-08-23-007; HH-2012-08-23-008; HH-2012-08-23-009b; HH-2012-08-23-010; HH-2012-08-23-011; HH-2012-08-23-012; HH-9739; HH-9912; HH-9914; HH-9918; HH-9919; HH-9951; HH-9952; Lake Heihai, Qinghai, China; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Sampling by hand
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
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  • 25
    Publication Date: 2023-03-13
    Keywords: Chlorophyll total; CTD/Rosette; CTD-RO; Dana01/16; Dana01/16_103; Dana01/16_104; Dana01/16_105; Dana01/16_106; Dana01/16_113; Dana01/16_114; Dana01/16_117; Dana01/16_118; Dana01/16_119; Dana01/16_127; Dana01/16_128; Dana01/16_129; Dana01/16_137; Dana01/16_138; Dana01/16_139; Dana01/16_141; Dana01/16_142; Dana01/16_148; Dana01/16_149; Dana01/16_150; Dana01/16_151; Dana01/16_160; Dana01/16_161; Dana01/16_162; Dana01/16_163; Dana01/16_171; Dana01/16_172; Dana01/16_177; Dana01/16_178; Dana01/16_179; Dana01/16_180; Dana01/16_186; Dana01/16_187; Dana01/16_188; Dana01/16_189; Dana01/16_197; Dana01/16_198; Dana01/16_199; Dana01/16_200; Dana01/16_207; Dana01/16_208; Dana01/16_209; Dana01/16_210; Dana01/16_213; Dana01/16_214; Dana01/16_215; Dana01/16_216; Dana II; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Kattegat; Latitude of event 2; Longitude of event; Nitrate; Nitrite; Nitrogen, total; Oxygen; Phosphate; Phosphorus, total; Pressure, water; Salinity; Silicate; Skagerrak; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2654 data points
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  • 26
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    Publication Date: 2023-03-13
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Latitude of event; Longitude of event; North Sea; Norwegian Sea; Pressure, water; Salinity; Scotia; Scotia16/1; Scotia16/1_10; Scotia16/1_11; Scotia16/1_12; Scotia16/1_13; Scotia16/1_14; Scotia16/1_15; Scotia16/1_16; Scotia16/1_17; Scotia16/1_18; Scotia16/1_19; Scotia16/1_20; Scotia16/1_21; Scotia16/1_22; Scotia16/1_23; Scotia16/1_24; Scotia16/1_25; Scotia16/1_26; Scotia16/1_27; Scotia16/1_28; Scotia16/1_29; Scotia16/1_30; Scotia16/1_31; Scotia16/1_32; Scotia16/1_33; Scotia16/1_34; Scotia16/1_35; Scotia16/1_36; Scotia16/1_37; Scotia16/1_38; Scotia16/1_39; Scotia16/1_40; Scotia16/1_41; Scotia16/1_42; Scotia16/1_43; Scotia16/1_44; Scotia16/1_45; Scotia16/1_46; Scotia16/1_47; Scotia16/1_48; Scotia16/1_49; Scotia16/1_50; Scotia16/1_51; Scotia16/1_52; Scotia16/1_53; Scotia16/1_9; South Atlantic Ocean; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2688 data points
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  • 27
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    PANGAEA
    In:  Institut für Meereskunde, Universität Hamburg
    Publication Date: 2023-03-10
    Keywords: cruise 02+03; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Event label; KJACK0107; KJACK2001_101; KJACK2001_102; KJACK2001_103; KJACK2001_104; KJACK2001_105; KJACK2001_106; KJACK2001_107; KJACK2001_108; KJACK2001_109; KJACK2001_110; KJACK2001_111; KJACK2001_112; KJACK2001_113; KJACK2001_114; KJACK2001_115; KJACK2001_116; KJACK2001_117; KJACK2001_118; KJACK2001_119; KJACK2001_120; KJACK2001_121; KJACK2001_122; KJACK2001_123; KJACK2001_124; KJACK2001_125; KJACK2001_126; KJACK2001_127; KJACK2001_128; KJACK2001_129; KJACK2001_130; KJACK2001_131; KJACK2001_132; KJACK2001_133; KJACK2001_134; KJACK2001_135; KJACK2001_136; KJACK2001_137; KJACK2001_138; KJACK2001_139; KJACK2001_140; KJACK2001_141; KJACK2001_142; KJACK2001_143; KJACK2001_144; KJACK2001_145; KJACK2001_146; KJACK2001_147; KJACK2001_148; KJACK2001_149; KJACK2001_150; KJACK2001_151; KJACK2001_152; KJACK2001_153; KJACK2001_154; KJACK2001_155; KJACK2001_156; KJACK2001_157; KJACK2001_158; KJACK2001_159; KJACK2001_160; KJACK2001_161; KJACK2001_162; KJACK2001_163; KJACK2001_164; KJACK2001_165; KJACK2001_166; KJACK2001_167; KJACK2001_169; KJACK2001_170; KJACK2001_171; KJACK2001_172; KJACK2001_173; KJACK2001_174; KJACK2001_175; KJACK2001_176; KJACK2001_177; KJACK2001_178; KJACK2001_179; KJACK2001_180; KJACK2001_181; KJACK2001_182; KJACK2001_183; KJACK2001_184; KJACK2001_185; KJACK2001_186; KJACK2001_187; KJACK2001_188; KJACK2001_189; KJACK2001_190; KJACK2001_191; KJACK2001_192; KJACK2001_193; KJACK2001_194; KJACK2001_195; KJACK2001_196; KJACK2001_197; KJACK2001_198; KJACK2001_199; KJACK2001_200; KJACK2001_201; KJACK2001_202; KJACK2001_203; KJACK2001_204; KJACK2001_205; KJACK2001_206; KJACK2001_207; KJACK2001_208; KJACK2001_209; KJACK2001_210; KJACK2001_211; KJACK2001_212; KJACK2001_213; KJACK2001_214; KJACK2001_215; KJACK2001_216; KJACK2001_217; KJACK2001_218; KJACK2001_219; KJACK2001_220; KJACK2001_221; KJACK2001_222; KJACK2001_223; KJACK2001_224; KJACK2001_225; KJACK2001_226; KJACK2001_227; KJACK2001_228; KJACK2001_229; KJACK2001_230; KJACK2001_231; KJACK2001_232; KJACK2001_233; KJACK2001_234; KJACK2001_235; KJACK2001_236; KJACK2001_237; KJACK2001_238; KJACK2001_239; KJACK2001_240; KJACK2001_241; KJACK2001_242; KJACK2001_243; KJACK2001_244; KJACK2001_245; KJACK2001_246; KJACK2001_247; KJACK2001_248; KJACK2001_249; KJACK2001_250; KJACK2001_251; KJACK2001_252; KJACK2001_253; KJACK2001_254; KJACK2001_255; KJACK2001_256; KJACK2001_257; KJACK2001_258; KJACK2001_259; KJACK2001_260; KJACK2001_261; KJACK2001_262; KJACK2001_263; KJACK2001_264; KJACK2001_265; KJACK2001_266; KJACK2001_267; KJACK2001_268; KJACK2001_269; KJACK2001_270; KJACK2001_271; Kommandor Jack; LATITUDE; LONGITUDE; Oxygen; Oxygen, dissolved; Pressure, water; Recalculated from ml/l by using (ml/l)*44.66; Salinity; South Atlantic Ocean; Temperature, water; UniHH_CTD
    Type: Dataset
    Format: text/tab-separated-values, 436810 data points
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  • 28
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    PANGAEA
    In:  Institut für Meereskunde, Universität Hamburg
    Publication Date: 2023-03-10
    Keywords: Chlorophyll a; Conductivity; CTD, Seabird; CTD/Rosette; CTD-R; CTD-RO; DATE/TIME; DEPTH, water; Elevation of event; Event label; LATITUDE; LONGITUDE; Pressure, water; Salinity; South Atlantic Ocean; Temperature, water; Transmission of light; UniHH_CTD; VA176; VA176_00-3; VA176_01-2; VA176_01-3; VA176_01-4; VA176_01-5; VA176_02; VA176_02-1; VA176_02-2; VA176_02-3; VA176_02-4; VA176_02-5; VA176_03; VA176_03-1; VA176_03-2; VA176_03-3; VA176_03-4; VA176_03-5; VA176_04; VA176_04-1; VA176_04-2; VA176_04-3; VA176_04-4; VA176_04-5; VA176_05; VA176_05-1; VA176_05-2; VA176_05-3; VA176_05-4; VA176_05-5; VA176_06; VA176_07; VA176_08; VA176_08-1; VA176_08-2; VA176_08-3; VA176_08-4; VA176_08-5; VA176_09; VA176_10; VA176_11; VA176_12; VA176_13; VA176_14; VA176_15; VA176_15-1; VA176_15-2; VA176_15-3; VA176_15-4; VA176_15-5; VA176_16; VA176_17; VA176_18; VA176_19; VA176_20; VA176_21; VA176_22; VA176_23; VA176_24; VA176_25; VA176_26; VA176_26-1; VA176_26-2; VA176_26-3; VA176_26-4; VA176_26-5; VA176_27; VA176_28; VA176_29; VA176_30; VA176_30-1; VA176_30-2; VA176_30-3; VA176_30-4; VA176_30-5; VA176_30-6; VA176_31; VA176_32; VA176_33; VA176_34; VA176_35; VA176_36; VA176_36-1; VA176_37; VA176_38; VA176_39; VA176_40; VA176_41; VA176_42; VA176_43; Valdivia (1961)
    Type: Dataset
    Format: text/tab-separated-values, 371658 data points
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  • 29
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    PANGAEA
    In:  Institut für Meereskunde, Universität Hamburg
    Publication Date: 2023-03-10
    Keywords: Conductivity; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; Greenland Sea; Latitude of event; Longitude of event; POS290; POS290_336; POS290_337; POS290_338; POS290_339; POS290_341; POS290_342; POS290_343; POS290_344; POS290_345; POS290_346; POS290_347; POS290_355; POS290_356; POS290_358; POS290_359; POS290_360; POS290_361; POS290_362; POS290_363; POS290_364; POS290_365; POS290_366; POS290_367; POS290_368; POS290_369; POS290_370; POS290_371; POS290_376; POS290_378; POS290_379; POS290_380; POS290_381; POS290_385; POS290_386; POS290_387; POS290_388; POS290_389; POS290_390; POS290_392; POS290_394; POS290_395; POS290_396; POS290_397; POS290_398; POS290_399; POS290_400; POS290_401; POS290_402; POS290_403; POS290_404; POS290_405; POS290_406; POS290_407; POS290_408; POS290_409; POS290_410; POS290_411; POS290_412; POS290_413; POS290_414; POS290_415; POS290_416; POS290_417; POS290_418; POS290_419; POS290_420; POS290_421; POS290_422; POS290_423; POS290_424; POS290_425; POS290_426; POS290_427; POS290_428; POS290_429; POS290_430; Poseidon; Pressure, water; Salinity; South Atlantic Ocean; Temperature, water; Transmission of light; UniHH_CTD
    Type: Dataset
    Format: text/tab-separated-values, 688315 data points
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  • 30
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    PANGAEA
    In:  Institut für Meereskunde, Universität Hamburg
    Publication Date: 2023-03-10
    Keywords: Conductivity; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; KONTROL 85; Latitude of event; Longitude of event; Pressure, water; Salinity; South Atlantic Ocean; Temperature, water; UniHH_CTD; VA35; VA35_01; VA35_02; VA35_03; VA35_04; VA35_05; VA35_06; VA35_07; VA35_08; VA35_09; VA35_10; VA35_11; VA35_12; VA35_13; VA35_14; VA35_15; VA35_16; VA35_17; VA35_18; VA35_19; VA35_20; VA35_21; VA35_22; VA35_23; VA35_24; VA35_25; VA35_26; VA35_27; VA35_28; VA35_29; VA35_30; VA35_31; VA35_32; VA35_33; VA35_34; VA35_35; VA35_36; VA35_37; VA35_38; VA35_39; VA35_40; Valdivia (1961)
    Type: Dataset
    Format: text/tab-separated-values, 13808 data points
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  • 31
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    PANGAEA
    In:  Supplement to: Putranto, Thomas Triadi; Rüde, Thomas (2016): Hydrogeological model of an urban city in a coastal area, case study: Semarang, Indonesia. Indonesian Journal on Geoscience, 3(1), 17-27, https://doi.org/10.17014/ijog.3.1.17-27
    Publication Date: 2023-03-14
    Description: In Semarang City, groundwater has been exploited as a natural resource since 1841. The groundwater exploited in deep wells is concentrated in confined aquifers. The previous hydrogeological model was developed in one unit of aquifer and refined then by using several hydrostratigraphical units following a regional hydrogeological map without any further analysis. At present, there is a lack of precise hydrogeological model which integrates geological and hydrogeological data, in particular for multiple aquifers in Semarang. Thus, the aim of this paper is to develop a hydrogeological model for the multiple aquifers in Semarang using an integrated data approach. Groundwater samples in the confined aquifers have been analyzed to define the water type and its lateral distribution. Two hydrogeological cross sections were then created based on several borelog data to define a hydrostratigraphical unit (HSU). The HSU result indicates the hydrogeological model of Semarang consists of two aquifers, three aquitards, and one aquiclude. Aquifer 1 is unconfined, while Aquifer 2 is confined. Aquifer 2 is classified into three groups (2a, 2b, and 2c) based on analyses of major ion content and hydrostratigraphical cross sections.
    Keywords: Aquifer type; Area/locality; Balance; Bicarbonate ion; Calcium; Calculated; Chloride; Conductivity, electrical; DATE/TIME; Depth, well; ELEVATION; Event label; Facies name/code; Handheld GPS, Garmin; Java Island, northern coast; Latitude of event; Longitude of event; Magnesium; N_1; N_2; N_3; N_7; pH; Portable water detector; Portable water quality meter (Hanna Instruments); Potassium; Sample position; Sampling Well; SB_100; SB_112; SB_120; SB_176; SB_185; SB_189; SB_190; SB_198; SB_206; SB_210; SB_211; SB_213; SB_214; SB_215; SB_217; SB_219; SB_220; SB_225; SB_226; SB_235; SB_256; SB_262; SB_265; SB_270; SB_271; SB_273; SB_278; SB_281; SB_282; SB_283; SB_297; SB_299; SB_321; SB_325; SB_33; SB_332; SB_344; SB_347; SB_348; SB_36; SB_590; SB_60; SB_726; SB_758; SB_790; SB_793; SB_92; SB_951; Sodium; SP_136; SP_138; SP_139; SP_341; SP_342; SP_764; Spectrophotometric; Sulfate; Total dissolved solids; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator; Water level; WELL
    Type: Dataset
    Format: text/tab-separated-values, 1131 data points
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  • 32
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    PANGAEA
    In:  Alfred Wegener Institute - Research Unit Potsdam
    Publication Date: 2023-03-14
    Keywords: 06-CYak-01; 06-CYak-02; 06-CYak-03; 06-CYak-04; 06-CYak-05; 06-NYak-01; 06-NYak-02; 06-NYak-03; 06-NYak-04; 06-NYak-05; 06-NYak-06; 06-NYak-07; 06-NYak-08; 06-NYak-09; 06-NYak-10; 06-NYak-11; 06-NYak-12; 06-NYak-13; 06-NYak-14; 06-NYak-15; Alaas; AWI_PerDyn; AWI Arctic Land Expedition; Ayan; Central Yakutia, Russia; Chat; Comment of event; Conductivity; Date/Time of event; Depth of Secchi Disk; Dulla; Etektyak; Event label; Ilimniir; Ivanovka; Kerdugen; Ketitiki; Krestyak; Latitude of event; Longitude of event; MULT; Multiple investigations; Nami-Kuel; North_Yakutia_2006; North Yakutia, Russia; Oibon-Kuel; Oloror; Oppoyao; Optional event label; Otto; Oxygen; Oxygen saturation; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2006_Yakutia; Spasskoe; Suturuoka; Temperature, water; Thee-Bihii; Timpi; Ushepes
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 33
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    PANGAEA
    In:  Alfred Wegener Institute - Research Unit Potsdam
    Publication Date: 2023-03-14
    Keywords: 09-TIK-01; 09-TIK-02; 09-TIK-03; 09-TIK-04; 09-TIK-05; 09-TIK-08; 09-TIK-09; 09-TIK-10; 09-TIK-11; 09-TIK-12; 09-TIK-13; 09-TIK-14; Alkalinity, total; AWI_PerDyn; AWI Arctic Land Expedition; Byluyng Kjuel; Comment of event; Conductivity; Date/Time of event; Depth of Secchi Disk; Elgene Kjuel; Event label; Latitude of event; Longitude of event; MULT; Multiple investigations; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2009_Lena-transect; Tiksi2009; Vegetation type
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
    Location Call Number Expected Availability
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  • 34
    Publication Date: 2023-03-14
    Keywords: 90BYBA40; 90BYBA40-track; Chlorophyll a; Chlorophyll b; Chlorophyll c; CT; Dalniye Zelentsy; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 7172 data points
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  • 35
    Publication Date: 2023-03-14
    Keywords: 90PD9E40; 90PD9E40-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 4574 data points
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  • 36
    Publication Date: 2023-03-14
    Keywords: 90DI9D20; 90DI9D20-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1941 data points
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  • 37
    Publication Date: 2023-03-14
    Keywords: 90PD9F70; 90PD9F70-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 380 data points
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  • 38
    Publication Date: 2023-03-14
    Keywords: 90PD9F50; 90PD9F50-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1018 data points
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  • 39
    Publication Date: 2023-03-14
    Keywords: 90PD9F80; 90PD9F80-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 9627 data points
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  • 40
    Publication Date: 2023-03-14
    Keywords: 90SBC810; 90SBC810-track; Ammonium; Coastal station Kola Bay; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 2939 data points
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  • 41
    Publication Date: 2023-03-14
    Keywords: 90XX9BA0; 90XX9BA0-track; Alkalinity, total; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 282 data points
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  • 42
    Publication Date: 2023-03-14
    Keywords: 90XX9C20; 90XX9C20-track; Alkalinity, total; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 283 data points
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  • 43
    Publication Date: 2023-03-14
    Keywords: 34AR9D7A; 34AR9D7A-track; Alkalinity, total; Ammonium; Aranda (1953); CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; pH; Phosphate; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 5073 data points
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  • 44
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    PANGAEA
    In:  Supplement to: Endres, Sonja; Galgani, Luisa; Riebesell, Ulf; Schulz, Kai Georg; Engel, Anja (2014): Stimulated Bacterial Growth under Elevated pCO2: Results from an Off-Shore Mesocosm Study. PLoS ONE, 9(6), e99228, https://doi.org/10.1371/journal.pone.0099228
    Publication Date: 2023-03-14
    Description: Marine bacteria are the main consumers of freshly produced organic matter. Many enzymatic processes involved in the bacterial digestion of organic compounds were shown to be pH sensitive in previous studies. Due to the continuous rise in atmospheric CO2 concentration, seawater pH is presently decreasing at a rate unprecedented during the last 300 million years but the consequences for microbial physiology, organic matter cycling and marine biogeochemistry are still unresolved. We studied the effects of elevated seawater pCO2 on a natural plankton community during a large-scale mesocosm study in a Norwegian fjord. Nine Kiel Off-Shore Mesocosms for Future Ocean Simulations (KOSMOS) were adjusted to different pCO2 levels ranging initially from ca. 280 to 3000 µatm and sampled every second day for 34 days. The first phytoplankton bloom developed around day 5. On day 14, inorganic nutrients were added to the enclosed, nutrient-poor waters to stimulate a second phytoplankton bloom, which occurred around day 20. Our results indicate that marine bacteria benefit directly and indirectly from decreasing seawater pH. During the first phytoplankton bloom, 5-10% more transparent exopolymer particles were formed in the high pCO2 mesocosms. Simultaneously, the efficiency of the protein-degrading enzyme leucine aminopeptidase increased with decreasing pH resulting in up to three times higher values in the highest pCO2/lowest pH mesocosm compared to the controls. In general, total and cell-specific aminopeptidase activities were elevated under low pH conditions. The combination of enhanced enzymatic hydrolysis of organic matter and increased availability of gel particles as substrate supported up to 28% higher bacterial abundance in the high pCO2 treatments. We conclude that ocean acidification has the potential to stimulate the bacterial community and facilitate the microbial recycling of freshly produced organic matter, thus strengthening the role of the microbial loop in the surface ocean.
    Keywords: Abundance per volume; BIOACID; Biological Impacts of Ocean Acidification; Chlorophyll a; DATE/TIME; Day of experiment; KOSMOS_2011_Bergen; Leucine aminopeptidase activity; MESO; Mesocosm experiment; pH; Raunefjord; Sample code/label; Transparent exopolymer particles as Gum Xanthan equivalents per volume; Transparent exopolymer particles as Gum Xanthan equivalents per volume, std dev
    Type: Dataset
    Format: text/tab-separated-values, 2053 data points
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  • 45
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    PANGAEA
    In:  Supplement to: Asmala, Eero; Haraguchi, Lumi; Markager, Stiig; Massicotte, Philippe; Riemann, Bo; Staehr, Peter A; Carstensen, Jacob (2018): Eutrophication leads to accumulation of recalcitrant autochthonous organic matter in coastal environment. Global Biogeochemical Cycles, 32(11), 1673-1687, https://doi.org/10.1029/2017GB005848
    Publication Date: 2023-03-14
    Description: Anthropogenic nutrient enrichment is changing the structure and the function of coastal ecosystems. These coastal zones are transitions between freshwater and marine systems where multiple biogeochemical processes remove, produce and transform organic matter. The extent to which the coastal zone is merely a conduit for terrestrial (allochthonous) organic matter, versus a distinct source of autochthonous organic matter fueled by eutrophication, is unclear. To address this issue, we characterized the freshwater and marine dissolved organic matter (DOM) pools in an eutrophic estuary with a long water residence time (Roskilde Fjord, Denmark) over an annual cycle. We combined elemental, optical (absorbance and fluorescence) and isotopic analyses to obtain insight about the bulk properties of the DOM pool during this period. We also used sediment traps to analyze the changes related to the exchange of organic matter between the particulate (POM) and dissolved (DOM) fractions. The results showed that labile autochthonous DOM from in situ primary production was rapidly transformed to more recalcitrant DOM that accumulated in the estuary despite continuous exchange with the open sea. Also, parts of the POM pool were degraded rapidly (within 24h) and transformed into the DOM pool. Accumulated DOM was characterized by relatively low molecular size and stable carbon isotopic value, and by high protein-like fluorescence. These results indicate that autotrophic material can be a major source of specific recalcitrant DOM in eutrophic coastal waters, contributing significantly to the flux of organic carbon to the ocean.
    Keywords: Absorption coefficient, 230 nm; Absorption coefficient, 254 nm; Absorption coefficient, 275 nm; Absorption coefficient, 295 nm; Absorption coefficient, 300 nm; Absorption coefficient, 350 nm; Absorption coefficient, 355 nm; Absorption coefficient, 375 nm; Absorption coefficient, 400 nm; Absorption coefficient, 440 nm; Ammonium; Biological index; Carbon, organic, dissolved; Carbon, organic, total; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Event label; Fluorescence, peak A; Fluorescence, peak C; Fluorescence, peak M; Fluorescence, peak T; Fluorescence index; Humification index; LATITUDE; LONGITUDE; Molecular mass; MULT; Multiple investigations; Nitrate; Nitrate and Nitrite; Nitrite; Nitrogen, inorganic, dissolved; Nitrogen, organic, dissolved; Nitrogen, total; Nitrogen, total dissolved; PDZ Europa ANCA-GSL elemental analyser; pH; Phosphate; Phosphorus, inorganic, dissolved; Phosphorus, organic, dissolved; Phosphorus, total; Phosphorus, total dissolved; Ratio; Roskilde_fjord_RF01; Roskilde_fjord_RF02; Roskilde_fjord_RF03; Roskilde_fjord_RF04; Roskilde_fjord_RF05; Roskilde_fjord_RF06; Roskilde_fjord_RF07; Roskilde_fjord_RF08; Salinity; Sample ID; SEC analyser; Silicate; Specific ultraviolet absorbance normalized to DOC, 254 nm; Spectral slope, 275-295 nm; Spectral slope, 300-650 nm; Spectral slope, 350-400 nm; Spectrophotometer UV/VIS (Shimadzu 2401PC); Temperature, water; Varian Cary Eclipse fluorometer (Agilent); Wet oxidation total organic carbon analyzer Shimadzu; δ13C, dissolved organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 7907 data points
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  • 46
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    PANGAEA
    In:  Supplement to: Juhlke, Tobias René; van Geldern, Robert; Huneau, Frédéric; Garel, Emilie; Santoni, Sébastien; Hemmerle, Hannes; Barth, Johannes A C (2019): Riverine carbon dioxide evasion along a high-relief watercourse derived from seasonal dynamics of the water-atmosphere gas exchange. Science of the Total Environment, 657, 1311-1322, https://doi.org/10.1016/j.scitotenv.2018.12.158
    Publication Date: 2023-03-14
    Description: The high-relief catchment of the Tavignanu River (Corsica Island, France) with an elevation range from sea level to 2622 m above sea level was investigated from January 2016 to April 2017 for its on-site parameters (T, pH, EC, TA), riverine carbon budget (TCO2) and stable carbon isotopes (d13C). Partial pressure of CO2 (pCO2) and annual carbon flux across the air-water boundary (FCO2) were calculated from analytical results. This data set contains the supplementary analytical data of the related publication.
    Keywords: Alkalinity, total; Carbon, inorganic, total; Carbon dioxide, flux; Carbon dioxide, flux, standard deviation; Carbon dioxide, partial pressure; Carbon dioxide, partial pressure, standard deviation; Conductivity, electrical; DATE/TIME; Distance; Elevation of event; Event label; I_Orta; II_Zincaghju; III_Vechju; IV_Corsigliese; Latitude of event; Longitude of event; pH; Restonica_R1; Restonica_R2; Restonica_R3; Restonica_R4; Restonica_R5; Restonica_R6; Site; Tavignanu_1; Tavignanu_10; Tavignanu_2; Tavignanu_3; Tavignanu_4; Tavignanu_5; Tavignanu_6; Tavignanu_7; Tavignanu_8; Tavignanu_9; Temperature, water; V_Tagnone; Water sample; WS; δ13C, dissolved inorganic carbon
    Type: Dataset
    Format: text/tab-separated-values, 920 data points
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  • 47
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St1; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 23155 data points
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  • 48
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St3; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 9960 data points
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  • 49
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St1; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 12530 data points
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  • 50
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20130904; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 31030 data points
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  • 51
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St4; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 1635 data points
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  • 52
    Publication Date: 2023-03-14
    Keywords: Acid titration; Area/locality; Aufsess; Bicarbonate ion; Calcium; Chloride; Conductivity, electrolytic; DATE/TIME; Distance; Ion chromatography; Kainach; LATITUDE; Leinleiter; LONGITUDE; Magnesium; Nitrate; Oxygen; pH; Phosphate; Potassium; Puettlach; Sample ID; Site; Sodium; Southern Germany; Sulfate; Temperature, water; Trubach; Truppach; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 590 data points
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  • 53
    Publication Date: 2023-03-14
    Keywords: Acid titration; Area/locality; Bicarbonate ion; Calcium; Chloride; Conductivity, electrolytic; DATE/TIME; Distance; Ion chromatography; LATITUDE; LONGITUDE; Magnesium; Nitrate; Oxygen; pH; Phosphate; Potassium; Sample ID; Site; Sodium; Southern Germany; Sulfate; Temperature, water; Water sample; Wiesent_River; WS
    Type: Dataset
    Format: text/tab-separated-values, 1063 data points
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  • 54
    Publication Date: 2023-03-14
    Keywords: Ammonium; Bicarbonate ion; Carbon, inorganic, total; Carbon, organic, dissolved; Carbon, organic, particulate; Carbon, organic, total; Carbon, total; Carbon dioxide; Chlorophyll a; Conductivity, electrical; DATE/TIME; DEPTH, water; Flow velocity, water; Laguna_LaConceja; Location; MULT; Multiple investigations; Nitrate; Nitrite; Nitrogen, inorganic, total; Nitrogen, organic, dissolved; Nitrogen, organic, total; Nitrogen, total; Nitrogen, total dissolved; pH; Phosphorus, reactive soluble; Phosphorus, total; River discharge; River level; River width; Spain; Suspended particulate matter; Visibility; Volume
    Type: Dataset
    Format: text/tab-separated-values, 1963 data points
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  • 55
    Publication Date: 2023-03-14
    Keywords: Bicarbonate; Carbon dioxide; Carbon dioxide, flux; Carbon dioxide, gradient at air/water interface; Carbon dioxide, partial pressure; Carbon dioxide (water) partial pressure; DATE/TIME; DEPTH, water; Laguna_LaConceja; MULT; Multiple investigations; pH; Piston velocity; Salinity; Spain; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 315 data points
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  • 56
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Experiment day; Nitrate; Nitrite; Nitrogen, inorganic, dissolved; Nitrogen in ammonium; Number; pH; Phosphate; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 840 data points
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  • 57
    Publication Date: 2023-03-14
    Keywords: Aluminium; Automatic water sampler (ISCO 3700); AWI_PerDyn; AWS_ISCO; Barium 2+; Bicarbonate ion; Bromide; Calcium; Carbon, organic, dissolved; Chloride; Conductivity, electrical; DATE/TIME; Fluoride; Herschel Island, Yukon Territory, Canada; Ice_Creek_West; Iron; Magnesium; Manganese 2+; Nitrate; Permafrost Research (Periglacial Dynamics) @ AWI; pH; Phosphorus; Potassium; Sample code/label; Silicon; Sodium; Strontium 2+; Sulfate
    Type: Dataset
    Format: text/tab-separated-values, 1260 data points
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  • 58
    Publication Date: 2023-03-14
    Keywords: Aluminium; Automatic water sampler (ISCO 3700); AWI_PerDyn; AWS_ISCO; Barium 2+; Bicarbonate ion; Bromide; Calcium; Carbon, organic, dissolved; Chloride; Conductivity, electrical; DATE/TIME; Fluoride; Herschel Island, Yukon Territory, Canada; Ice_Creek_West; Iron; Magnesium; Manganese 2+; Nitrate; Nitrogen, total dissolved; Oxygen saturation; Permafrost Research (Periglacial Dynamics) @ AWI; pH; Phosphate; Phosphorus; Potassium; Sample code/label; Silicon; Sodium; Strontium 2+; Sulfate; Suspended particulate matter
    Type: Dataset
    Format: text/tab-separated-values, 896 data points
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  • 59
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Calculated; Carbon, inorganic, dissolved; Carbon dioxide, partial pressure; CO2 acid liberation; Conductivity, electrical; Czech Republic; DATE/TIME; Element analyser isotope ratio mass spectrometer (EA-IRMS); Elevation of event; Event label; Isotope ratio mass spectrometry; Latitude of event; Longitude of event; Multiparameter instrument; Original value; Oxidation reduction (RedOx) potential; Oxygen; Oxygen saturation; pH; Sample ID; Temperature, water; Uhlirska_DST; Uhlirska_HST; Uhlirska_P84; Water sample; WS; δ13C, dissolved inorganic carbon; δ13C, particulate organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 772 data points
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  • 60
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Calculated; Carbon, inorganic, dissolved; Carbon dioxide, partial pressure; CO2 acid liberation; Conductivity, electrical; Czech Republic; DATE/TIME; DEPTH, water; Element analyser isotope ratio mass spectrometer (EA-IRMS); Isotope ratio mass spectrometry; Multiparameter instrument; Original value; Oxidation reduction (RedOx) potential; Oxygen; Oxygen saturation; pH; River discharge; Sample ID; Temperature, water; Uhlirska_UHL; V-notch weir; Water sample; WS; δ13C, dissolved inorganic carbon; δ13C, particulate organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 855 data points
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  • 61
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Calcite saturation state; Calculated using CO2SYS; Carbonate ion; Carbon dioxide (water) partial pressure; DATE/TIME; Dry air column-averaged mixing ratio of carbon dioxide; Kristineberg_Loven-Centre; Number; Oxygen; pH; Research station; RS; Salinity; Sweden; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 404 data points
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  • 62
    Publication Date: 2023-03-14
    Keywords: Classification; Color, a*; Color, b*; Color, L*, lightness; Conductivity; DEPTH, sediment/rock; Elba; Elba_F-I; F-I; Gravel; Gravel classification according to Ad-Hoc-AG Boden 2005 (KA5); Hand-held checker, 1:2.5 sample:ddH2O solution; Hand-held checker, 1:2.5 sample:KCl solution; Loss on ignition; Magnetic susceptibility, frequency dependence; Magnetic susceptibility, frequency dependence, standard deviation; Magnetic susceptibility, low-field; MS2B sensor; pH; Portable spectrophotometer Minolta CM-2500d; VC; Vibro corer
    Type: Dataset
    Format: text/tab-separated-values, 1076 data points
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  • 63
    Publication Date: 2023-03-14
    Keywords: CHN +S analyser; Classification; Color, a*; Color, b*; Color, L*, lightness; Conductivity; DEPTH, sediment/rock; Elba; Elba_S-I; Gravel; Gravel classification according to Ad-Hoc-AG Boden 2005 (KA5); Hand-held checker, 1:2.5 sample:ddH2O solution; Hand-held checker, 1:2.5 sample:KCl solution; Loss on ignition; Magnetic susceptibility, frequency dependence; Magnetic susceptibility, frequency dependence, standard deviation; Magnetic susceptibility, low-field; MS2B sensor; pH; Portable spectrophotometer Minolta CM-2500d; S-I; Sulfur, total; VC; Vibro corer
    Type: Dataset
    Format: text/tab-separated-values, 1351 data points
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  • 64
    Publication Date: 2023-03-14
    Keywords: Africa, Ethiopia; Branched and isoprenoid tetraether index; Calculated; Cyclization ratio of branched tetraethers; DEPTH, soil; Depth, soil, maximum; Depth, soil, minimum; Elevation of event; Event label; I; II; III; IV; Jimma_zone_I; Jimma_zone_II; Jimma_zone_III; Jimma_zone_IV; Jimma_zone_V; Jimma_zone_VI; Land use; Methylation index of dominant branched tetraethers; MULT; Multiple investigations; Optional event label; pH; Temperature, annual mean; V; VI
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 65
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Autotitrator Metrohm 785 and electrode; Barium/Calcium ratio; Barium/Calcium ratio, standard deviation; Comment; Experiment; ICP-MS, Agilent 7500-ce; Number of observations; pH; Strontium-86/Strontium-88, standard deviation; Strontium-86/Strontium-88 ratio; Strontium-87/Strontium-88, standard deviation; Strontium-87/Strontium-88 ratio; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 98 data points
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  • 66
    Publication Date: 2023-03-14
    Keywords: Barium/Calcium ratio; Experiment; ICP-MS, Agilent 7500-ce; LA-ICP-MS, Laser-ablation inductively coupled plasma mass spectrometer; Neogloboquadrina dutertrei, Barium/Calcium ratio; pH; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 325 data points
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  • 67
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Carbon, inorganic, dissolved; Carbonate ion; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Ratio; Salinity; Sample code/label; Standard deviation; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 506 data points
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  • 68
    Publication Date: 2023-03-14
    Keywords: Acidity; Alkalinity, total; Ammonium; Area/locality; AWI_PerDyn; AWI_POK-02; AWI_POK-03; AWI_POK-04; AWI_POK-05; AWI_POK-06; AWI_POK-07; AWI_POK-08; AWI_POK-09; AWI_POK-10; AWI_POK-11; AWI_POK-12; AWI_POK-13; AWI_POK-14; AWI_POK-15; AWI_POK-16; AWI_POK-17; AWI_POK-18; AWI_POK-19; AWI_POK-20; AWI_POK-21; AWI_POK-22; AWI_POK-23; AWI_POK-24; AWI_POK-25; AWI_POK-26; AWI_POK-27; AWI_POK-28; AWI_POK-29; AWI_POK-30; AWI_POK-31; AWI Arctic Land Expedition; Bottom water temperature; Comment; Conductivity, electrolytic; DATE/TIME; Depth, bottom/max; Event label; Hardness description; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Nitrate; Oxygen; Permafrost Research (Periglacial Dynamics) @ AWI; pH; Phosphate; RU-Land_2012_Kytalyk_Kolyma; Sampling/measurement on land; Siberia, Russia; Size; Temperature, air; Temperature, water; Type
    Type: Dataset
    Format: text/tab-separated-values, 445 data points
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  • 69
    Publication Date: 2023-03-14
    Keywords: AWI_PerDyn; AWI Arctic Land Expedition; Conductivity, electrolytic; DEPTH, sediment/rock; Description; Distance; East Siberia; Height; Ice content; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Permafrost Research (Periglacial Dynamics) @ AWI; pH; pingo_exposure; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sample type; Sampling/measurement on land; Shirokovsky_Kholm
    Type: Dataset
    Format: text/tab-separated-values, 437 data points
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  • 70
    Publication Date: 2023-03-14
    Keywords: AWI_L-24; AWI_L-25; AWI_L-31; AWI_L-34; AWI_L-36; AWI_L-38; AWI_L-6; AWI_L-62; AWI_L-66; AWI_L-80; AWI_PerDyn; AWI Arctic Land Expedition; Conductivity, electrical; DATE/TIME; DEPTH, water; Event label; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sampling/measurement on land; Siberia, Russia
    Type: Dataset
    Format: text/tab-separated-values, 70 data points
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  • 71
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St2; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 19395 data points
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  • 72
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St2; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 10530 data points
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  • 73
    Publication Date: 2023-03-14
    Keywords: 9038B970; 9038B970-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Pomor; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1000 data points
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  • 74
    Publication Date: 2023-03-14
    Keywords: 90BYB8C0; 90BYB8C0-track; CT; Dalniye Zelentsy; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; Oxygen; Oxygen saturation; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1307 data points
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  • 75
    Publication Date: 2023-03-14
    Keywords: 90BYBA60; 90BYBA60-track; Chlorophyll a; Chlorophyll b; Chlorophyll c; CT; Dalniye Zelentsy; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; Oxygen; Oxygen saturation; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1687 data points
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  • 76
    Publication Date: 2023-03-14
    Keywords: 90DI9CA0; 90DI9CA0-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1181 data points
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  • 77
    Publication Date: 2023-03-14
    Keywords: 90DI9D10; 90DI9D10-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 929 data points
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  • 78
    Publication Date: 2023-03-14
    Keywords: 90DI9CB0; 90DI9CB0-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1623 data points
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  • 79
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Description: This data set was collected during the R. V. Polarstern cruise PS82. Outside territorial waters, current velocities were measured nearly continuously along the ship's track with a vessel-mounted TRD Instruments 153.6-kHz Ocean Surveyor ADCP. The transducers were located 11 meters below the water line and were protected against ice floes by an acoustically transparent plastic window. The current measurements used a pulse of 2 seconds and vertical bin length of 4 meters. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). Heading, roll and pitch data from the ship's gyro platforms and the navigation data were used to convert the ADCP velocities into earth coordinates. The accuracy of the ADCP velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. The ADCP data were processed using the Ocean Surveyor Sputum Interpreter (OSSI) software developed by GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel. The reference layer was set to avoid near surface effects. The averaging interval was set to 120 seconds. Sampling interval setting: 2s; Number of bins: 80; Bin length: 4m; Pulse length: 4m; Blank beyond transmit length: 4m. Data processing setting: Upper depth of reference layer: 30m; Lower depth of reference layer: 80m; Time average: 120s; Misalignment angle: 0.9200 (from 2014-01-01T09:22:00 to 2014-02-04T15:34:00 Misalignment angle: 0.8600); amplitude: 1.0225. The precision for single ping and 4m cell size reported by TRDI is 0.30m/s. Resulting from the single ping precision and the number of pings (most of the time 36) during 120seconds the velocity accuracy is nearly 0.05m/s. (Velocity accuracy = single ping precision divided by square root of the number of pings).
    Keywords: Acoustic Doppler Current Profiling (ADCP), TRDI Ocean Surveyor, 153.6 kHz; ANT-XXIX/9; AWI_PhyOce; CT; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Physical Oceanography @ AWI; Polarstern; PS82; PS82-track; Quality; Underway cruise track measurements; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 8047893 data points
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  • 80
    Publication Date: 2023-03-16
    Keywords: Age, 14C; Age, dated; ANT-XXV/1; ANT-XXV/2; AWI_EcolChem; AWI_MarGeoChem; Canarias Sea; Carbon, organic, dissolved; Carbon, organic, dissolved, extracted; Celtic Sea; Center for Marine Environmental Sciences; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Ecological Chemistry @ AWI; English Channel; Event label; LATITUDE; LONGITUDE; Marine Geochemistry @ AWI; MARUM; Nitrogen, organic, dissolved, extracted; Polarstern; PS73; PS73/002-1; PS73/004-1; PS73/006-1; PS73/006-3; PS73/008-1; PS73/010-2; PS73/013-1; PS73/015-1; PS73/015-2; PS73/017-2; PS73/019-1; PS73/022-1; PS73/024-1; PS73/026-1; PS73/026-2; PS73/028-1; PS73/030-1; PS73/032-1; PS73/032-4; PS73/034-1; PS73/036-1; PS73/038-1; PS73/038-2; PS73/042-1; PS73/044-1; PS73/047-1; PS73/051-1; PS73/054-1; PS73/056-1; PS73/062-1; PS73/064-1; PS73/069-2; PS73/070-1; PS73/071-1; PS73/072-1; PS73/073-1; PS73/074-1; PS73/S10; PS73/S11; PS73/S13; PS73/S15; PS73/S16; PS73/S17; PS73/S19; PS73/S2; PS73/S21; PS73/S24; PS73/S26; PS73/S29; PS73/S3; PS73/S30; PS73/S32; PS73/S34; PS73/S36; PS73/S38; PS73/S41; PS73/S43; PS73/S44; PS73/S45; PS73/S46; PS73/S47; PS73/S49; PS73/S5; PS73/S50; PS73/S52; PS73/S55; PS73/S57; PS73/S58; PS73/S60; PS73/S66; PS73/S67; PS73/S68; PS73/S69; PS73/S7; PS73/S70; PS73/S71; PS73/SW1; PS73/SW10; PS73/SW11; PS73/SW12; PS73/SW13; PS73/SW14; PS73/SW15; PS73/SW16; PS73/SW17; PS73/SW18; PS73/SW19; PS73/SW2; PS73/SW3; PS73/SW4; PS73/SW5; PS73/SW6; PS73/SW7; PS73/SW8; PS73/SW9; RAMSES; RAMSES hyperspectral radiometer; Solid phase extraction (SPE) with PPL sorbent (after Flerus et al. 2012); South Atlantic Ocean; Station label; Sulfur, organic, dissolved, extracted; Sulfur, organic, dissolved/Nitrogen, organic, dissolved ratio; Surface water sample; SWS; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1234 data points
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  • 81
    Publication Date: 2023-03-16
    Keywords: ANT-XXV/1; ANT-XXV/2; Area/locality; AWI_EcolChem; AWI_MarGeoChem; Canarias Sea; Celtic Sea; Center for Marine Environmental Sciences; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Double bond equivalent; Ecological Chemistry @ AWI; English Channel; Event label; Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR-MS); Hydrogen/Carbon ratio; LATITUDE; LONGITUDE; Marine Geochemistry @ AWI; MARUM; Mass of molecular formulas; Nitrogen/Carbon ratio; Oxygen/Carbon ratio; Polarstern; PS73; PS73/002-1; PS73/004-1; PS73/006-1; PS73/006-3; PS73/008-1; PS73/010-2; PS73/013-1; PS73/015-1; PS73/015-2; PS73/017-2; PS73/019-1; PS73/022-1; PS73/024-1; PS73/026-1; PS73/026-2; PS73/028-1; PS73/030-1; PS73/032-1; PS73/032-4; PS73/034-1; PS73/036-1; PS73/038-1; PS73/038-2; PS73/042-1; PS73/044-1; PS73/047-1; PS73/051-1; PS73/054-1; PS73/056-1; PS73/064-1; PS73/069-2; PS73/070-1; PS73/071-1; PS73/072-1; PS73/073-1; PS73/074-1; PS73/S10; PS73/S11; PS73/S13; PS73/S15; PS73/S16; PS73/S17; PS73/S19; PS73/S2; PS73/S21; PS73/S24; PS73/S26; PS73/S29; PS73/S3; PS73/S30; PS73/S32; PS73/S34; PS73/S36; PS73/S38; PS73/S41; PS73/S43; PS73/S44; PS73/S45; PS73/S46; PS73/S47; PS73/S49; PS73/S5; PS73/S52; PS73/S55; PS73/S57; PS73/S58; PS73/S60; PS73/S66; PS73/S67; PS73/S68; PS73/S69; PS73/S7; PS73/S70; PS73/S71; PS73/SW1; PS73/SW10; PS73/SW11; PS73/SW12; PS73/SW13; PS73/SW14; PS73/SW15; PS73/SW16; PS73/SW17; PS73/SW18; PS73/SW19; PS73/SW2; PS73/SW3; PS73/SW4; PS73/SW5; PS73/SW6; PS73/SW7; PS73/SW8; PS73/SW9; RAMSES; RAMSES hyperspectral radiometer; South Atlantic Ocean; Station label; Sulfur/Carbon ratio; Surface water sample; SWS; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1400 data points
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  • 82
    Publication Date: 2023-03-16
    Keywords: ANT-XXV/1; ANT-XXV/2; Area/locality; AWI_EcolChem; AWI_MarGeoChem; Canarias Sea; Center for Marine Environmental Sciences; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Ecological Chemistry @ AWI; Event label; LATITUDE; LONGITUDE; Marine Geochemistry @ AWI; MARUM; Methionine; Polarstern; PS73; PS73/026-1; PS73/026-2; PS73/073-1; Solid phase extraction (SPE) with PPL sorbent (after Flerus et al. 2012); Station label; Sulfur, organic, dissolved, extracted; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 83
    Publication Date: 2023-03-16
    Keywords: ANT-XXIII/2; AWI_PhyOce; AWI229-7; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS69; Weddell Sea
    Type: Dataset
    Format: application/zip, 285.7 MBytes
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  • 84
    Publication Date: 2023-03-16
    Keywords: ANT-XXIII/2; AWI_PhyOce; AWI231-7; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS69; Weddell Sea
    Type: Dataset
    Format: application/zip, 287.1 MBytes
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  • 85
    Publication Date: 2023-03-16
    Keywords: ANT-XXIII/2; AWI_PhyOce; AWI232-8; Mooring (long time); MOORY; Physical Oceanography @ AWI; Polarstern; PS69; Weddell Sea
    Type: Dataset
    Format: application/zip, 306.2 MBytes
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  • 86
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/019-6; Sea Ice Physics @ AWI; Transflectance; 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 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 2916400 data points
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  • 87
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/027-2; Sea Ice Physics @ AWI; Transflectance; 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 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 2357212 data points
    Location Call Number Expected Availability
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  • 88
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/039-6; Sea Ice Physics @ AWI; Transflectance; 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 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 512272 data points
    Location Call Number Expected Availability
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  • 89
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/031-2; Sea Ice Physics @ AWI; Transflectance; 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 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 4226244 data points
    Location Call Number Expected Availability
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  • 90
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/043-4; Sea Ice Physics @ AWI; Transflectance; 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 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 2783260 data points
    Location Call Number Expected Availability
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  • 91
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/046-1; Sea Ice Physics @ AWI; Transflectance; 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 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 687256 data points
    Location Call Number Expected Availability
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  • 92
    Publication Date: 2023-03-16
    Keywords: Arctic Ocean; ARK-XXIX/1, TRANSSIZ; AWI_SeaIce; Calculated; DATE/TIME; DEPTH, water; Distance, relative, X; Distance, relative, Y; ICE; Ice station; Polarstern; PS92; PS92/047-3; Sea Ice Physics @ AWI; Transflectance; 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 nm; Transflectance at 616 nm; Transflectance at 617 nm; Transflectance at 618 nm;
    Type: Dataset
    Format: text/tab-separated-values, 3376684 data points
    Location Call Number Expected Availability
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  • 93
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; ANT-XXXI/4; AWI_Meteo; Humidity, relative; Meteorological Long-Term Observations @ AWI; Polarstern; Pressure, at given altitude; PS98; PS98/38786; RADIO; Radiosonde; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6125 data points
    Location Call Number Expected Availability
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  • 94
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; ANT-XXXI/4; AWI_Meteo; Humidity, relative; Meteorological Long-Term Observations @ AWI; Polarstern; Pressure, at given altitude; PS98; PS98/38788; RADIO; Radiosonde; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6780 data points
    Location Call Number Expected Availability
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  • 95
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; ANT-XXXI/4; AWI_Meteo; Humidity, relative; Meteorological Long-Term Observations @ AWI; Polarstern; Pressure, at given altitude; PS98; PS98/38794; RADIO; Radiosonde; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 5790 data points
    Location Call Number Expected Availability
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  • 96
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ALTITUDE; ANT-XXXI/4; AWI_Meteo; Humidity, relative; Meteorological Long-Term Observations @ AWI; Polarstern; Pressure, at given altitude; PS98; PS98/38796; RADIO; Radiosonde; South Atlantic Ocean; Temperature, air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6480 data points
    Location Call Number Expected Availability
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  • 97
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_f_06; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-07-13
    Type: Dataset
    Format: text/tab-separated-values, 73203 data points
    Location Call Number Expected Availability
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  • 98
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_m_03; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-03-13
    Type: Dataset
    Format: text/tab-separated-values, 26429 data points
    Location Call Number Expected Availability
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  • 99
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_f_01; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-01-13
    Type: Dataset
    Format: text/tab-separated-values, 41145 data points
    Location Call Number Expected Availability
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  • 100
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_f_05; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-05-13
    Type: Dataset
    Format: text/tab-separated-values, 18369 data points
    Location Call Number Expected Availability
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