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  • Adolf Jensen; AJ_200605; AJ_FB1; AJ_FB1.5; AJ_FB2; AJ_FB2.5; AJ_FB3; AJ_FB3.5; AJ_FB4; AJ_GF1; AJ_GF10; AJ_GF13; AJ_GF2; AJ_GF3; AJ_GF5; AJ_GF7; Copepoda, eggs, production as carbon; Copepoda, production of carbon; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Estimated, after Hirst & Bunker (2003); Event label; Fyllas Banke, West Greenland; Godthåbsfjord, West Greenland; International Polar Year (2007-2008); IPY; Latitude of event; Longitude of event; MULT; Multiple investigations; Station label  (1)
  • Binary Object; Binary Object (File Size); Binary Object (MD5 Hash); Binary Object (Media Type); CTD/Rosette; CTD-RO; Date/Time of event; East Greenland; Elevation of event; Event label; File content; Glacier meltwater runoff; HDMS Knud Rasmussen; KN_2021; KR21044; KR21045; KR21046; KR21047; KR21048; KR21049; KR21050; KR21051; KR21052; KR21053; KR21054; KR21056; KR21057; KR21060; KR21061; KR21062; KR21063; KR21072; Labrador Sea; Latitude of event; Longitude of event; meteoric; water masses  (1)
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  • 1
    facet.materialart.
    Unknown
    (Table 2) Copepod carbon production in the upper 50 m in Godthabsfjord and Fyllas Banke, West Greenland (2010)
    PANGAEA
    In:  Supplement to: Arendt, Kristine Engel; Nielsen, Torkel Gissel; Rysgaard, Søren; Tönnesson, Kajsa (2010): Differences in plankton community structure along the Godthabsfjord, from the Greenland Ice Sheet to offshore waters. Marine Ecology Progress Series, 401, 49-62, https://doi.org/10.3354/meps08368
    Details
    Publication Date: 2024-01-24
    Description: This study describes differences in plankton community structure and in chemical and physical gradients between the offshore West Greenland Current system and inland regions close to the Greenland Ice Sheet during the post-bloom in Godthabsfjorden (64° N, 51° W). The offshore region had pronounced vertical mixing, with centric diatoms and Phaeocystis spp. dominating the phytoplankton, chlorophyll (chl) a (0.3 to 3.9 µg/l) was evenly distributed and nutrients were depleted in the upper 50 m. Ciliates and heterotrophic dinoflagellates constituted equal parts of the protozooplankton biomass. Copepod biomass was dominated by Calanus spp. Primary production, copepod production and the vertical flux were high offshore. The water column was stratified in the fjord, causing chl a to be concentrated in a thin sub-surface layer. Nutrients were depleted above the pycnocline, and Thalassiosira spp. dominated the phytoplankton assemblage close to the ice sheet. Dinoflagellates dominated the protozooplankton biomass, whereas copepod biomass was low and was dominated by Pseudocalanus spp. and Metridia longa. Primary production was low in the outer part of the fjord but considerably higher in the inner parts of the fjord. Copepod production was exceeded by protozooplankton production in the fjord. The results of both physical/chemical factors and biological parameters suggest separation of offshore and fjord systems.
    Keywords: Adolf Jensen; AJ_200605; AJ_FB1; AJ_FB1.5; AJ_FB2; AJ_FB2.5; AJ_FB3; AJ_FB3.5; AJ_FB4; AJ_GF1; AJ_GF10; AJ_GF13; AJ_GF2; AJ_GF3; AJ_GF5; AJ_GF7; Copepoda, eggs, production as carbon; Copepoda, production of carbon; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Estimated, after Hirst & Bunker (2003); Event label; Fyllas Banke, West Greenland; Godthåbsfjord, West Greenland; International Polar Year (2007-2008); IPY; Latitude of event; Longitude of event; MULT; Multiple investigations; Station label
    Type: Dataset
    Format: text/tab-separated-values, 98 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 2
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    Unknown
    Raw data of summer hydrographic conditions at proglacial fjord entrances along East Greenland during HDMS Knud Rasmussen expedition KN_2021 in August 2021 (2024)
    PANGAEA
    Details
    Publication Date: 2024-04-20
    Description: Here we present results from a synoptic survey of the pan‐east Greenland coastal system from the entrance of fjords at Cape Farewell (59°N) to Kaiser Franz Josef Fjord (73°N). Using conductivity‐temperature‐depth (CTD) profiles and water isotopes (δ18O, δ2H) sampling, we aim to describe the spatial distribution of water masses and source water fractions along east Greenland and their link to proglacial fjords. This is a hydrographic dataset containing CTD cast from the HDMS Knud Rasmussen cruise KR_2021 that took place from 10-26 August 2021 and was part of the research project Greenland Gradients led by Rysgaard, Sören. On each station, vertical CTD (SBE19plus) casts were made down to 500 m water depth or close to the sea floor if shallower. Temperature and salinity data were derived from these CTD profiles. Temperature is reported as potential temperature (ITS-90, degree C).
    Keywords: Binary Object; Binary Object (File Size); Binary Object (MD5 Hash); Binary Object (Media Type); CTD/Rosette; CTD-RO; Date/Time of event; East Greenland; Elevation of event; Event label; File content; Glacier meltwater runoff; HDMS Knud Rasmussen; KN_2021; KR21044; KR21045; KR21046; KR21047; KR21048; KR21049; KR21050; KR21051; KR21052; KR21053; KR21054; KR21056; KR21057; KR21060; KR21061; KR21062; KR21063; KR21072; Labrador Sea; Latitude of event; Longitude of event; meteoric; water masses
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
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