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  • 1
    Publication Date: 2023-05-12
    Description: Freshwater in the Arctic Ocean plays an important role in the regional ocean circulation, sea ice, and global climate. From salinity observed by a variety of platforms, we are able, for the first time, to estimate a statistically reliable liquid freshwater trend from monthly gridded fields over all upper Arctic Ocean basins. From 1992 to 2012 this trend was 600±300 km**3/yr. A numerical model agrees very well with the observed freshwater changes. A decrease in salinity made up about two thirds of the freshwater trend and a thickening of the upper layer up to one third. The Arctic Ocean Oscillation index, a measure for the regional wind stress curl, correlated well with our freshwater time series. No clear relation to Arctic Oscillation or Arctic Dipole indices could be found. Following other observational studies, an increased Bering Strait freshwater import to the Arctic Ocean, a decreased Davis Strait export, and enhanced net sea ice melt could have played an important role in the freshwater trend we observed.
    Type: Dataset
    Format: 11 datasets
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Gerland, Sebastian; Lind, Bjørn; Dowdall, Mark; Karcher, Michael J; Kolstad, Anne Kathrine (2003): 99Tc in seawater in the West Spitsbergen Current and adjacent areas. Journal of Environmental Radioactivity, 69(1-2), 119-127, https://doi.org/10.1016/S0265-931X(03)00090-0
    Publication Date: 2023-10-28
    Description: 99Tc levels were measured in seawater samples collected between 2000 and 2002 in the West Spitsbergen Current (WSC) and along the western coast of Svalbard or Spitzbergen and compared with available oceanographic 3-D modelling results for the late 1990s. Additional data from related regions are also presented in order to support the data interpretation. The seawater in the Arctic fjord Kongsfjorden on the western coast of Svalbard is influenced by the WSC, as shown by the 99Tc levels in surface water. By means of the WSC, 99Tc reaches the Eastern Fram Strait, where one branch of the WSC turns west into the East Greenland Current (EGC), and another branch continues northwards into the Arctic Ocean. Surface seawater collected in the central part of the WSC during a cruise on board the R/V "Polarstern" in the summer of 2000, showed higher levels of 99Tc than samples measured in Kongsfjorden in the spring of 2000. However, all levels measured in surface water are of the same order of magnitude. Data from sampling of deeper water in the WSC and EGC provide information pertaining to the lateral distribution of 99Tc. In all vertical profiling surveys (conducted in spring and summer), the highest levels of 99Tc were found in surface water. Comparison with oceanographic 3-D modelling indicates both significant seasonal variations in the lateral stratification of the WSC and variations with depth over shorter vertical distances. This information can be applied in sampling strategies, environmental monitoring, long-range transport of pollutants and physical oceanography.
    Keywords: Arctic Ocean; Area/locality; ARK-XVI/2; around Svalbard; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; Giant water sampler; GWS; Latitude of event; Longitude of event; Polarstern; PS57; PS57/173-1; PS57/173-3; PS57/197-1; PS57/264-2; PS57/264-3; SV00-1b; SV00-2a; SV00-4b; SV01-11b; SV01-1c; SV01-9b; SV02-MS1; Technetium-99; Technetium-99, standard deviation; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-04-20
    Description: This dataset contains hydroacoustic measurements collected by an autonomous ice-tethered bio-physical observatory during its drift across the Central Arctic Ocean from the end of MOSAiC in September 2020 to the next spring in May 2021. The measurements were performed by an Acoustic Zooplankton and Fish Profiler (AZFP, ASL) with factory calibrations. Data are provided as volume backscatter (Sv, in dB re 1 m⁻¹). We provide data for the frequencies 67, 125, 200 and 455 kHz. These files contain the quality-controlled raw data. The data were cleaned, processed and analysed in the paper Sea-ice decline makes zooplankton stay deeper for longer by Flores, Veyssiere et al. (submitted to Nature Cliimate Change), which contains a detailed description of the instrument and the measurement settings. The format can be readily ingested in the hydroacoustic data processing application EchoView.
    Keywords: 2020AZFP1; Acoustical Zoological Fish Profiler; Arctic_PASSION; Arctic Ocean; AZFP; Binary Object; central Arctic Ocean; DATE/TIME; ECOLIGHT; Ecosystem functions controlled by sea ice and light in a changing Arctic; File content; FRAM; FRontiers in Arctic marine Monitoring; Hydroacoustic backscatter; LATITUDE; LONGITUDE; MIDO; Mosaic; MOSAiC; MOSAIC_PO; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Multidisciplinary Ice-based Distributed Observatory; Pan-Arctic observing System of Systems: Implementing Observations for societal Needs; Polarstern; PS122/5; PS122/5_58-163; vertical migration; Zooplankton
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
    Location Call Number Limitation Availability
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  • 4
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    Unknown
    Elsevier
    In:  In: Siberian River Run-Off in the Kara Sea: Characterization, Quantification, Variability and Environmental Significance. , ed. by Stein, R., Fahl, K., Fütterer, D., Galimov, E. M. and Stepanets, O. V. Proceedings in Marine Sciences, 6 . Elsevier, Amsterdam, pp. 47-72. ISBN 0-444-51365-5
    Publication Date: 2015-03-09
    Type: Book chapter , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
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