Poster Open Access
Wiedmann, Ingrid;
Svensen, Camilla;
Jonasdottir, Sigrun;
Dąbrowska, Anna;
Koski, Marja
<?xml version='1.0' encoding='UTF-8'?> <record xmlns="http://www.loc.gov/MARC21/slim"> <leader>00000nam##2200000uu#4500</leader> <datafield tag="041" ind1=" " ind2=" "> <subfield code="a">eng</subfield> </datafield> <controlfield tag="005">20230321110457.0</controlfield> <controlfield tag="001">7603091</controlfield> <datafield tag="711" ind1=" " ind2=" "> <subfield code="d">30 January - 2 February 2023</subfield> <subfield code="a">Arctic Frontiers Conference 2023</subfield> <subfield code="c">Tromsø, Norway</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="u">UiT The Arctic University of Norway</subfield> <subfield code="0">(orcid)0000-0001-9577-3935</subfield> <subfield code="a">Svensen, Camilla</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="u">Technical University of Denmark, Lyngby, Denmark</subfield> <subfield code="0">(orcid)0000-0003-4985-0447</subfield> <subfield code="a">Jonasdottir, Sigrun</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="u">Institute of Oceanology Polish Academy of Sciences, Sopot, Poland</subfield> <subfield code="0">(orcid)0000-0002-0911-3082</subfield> <subfield code="a">Dąbrowska, Anna</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="u">Technical University of Denmark, Lyngby, Denmark</subfield> <subfield code="0">(orcid)0000-0002-1860-9768</subfield> <subfield code="a">Koski, Marja</subfield> </datafield> <datafield tag="856" ind1="4" ind2=" "> <subfield code="s">1843579</subfield> <subfield code="z">md5:80ab62a0e14cf43db8c0d94899200884</subfield> <subfield code="u">https://zenodo.org/record/7603091/files/Poster_WiedmannIngrid_FINAL.pdf</subfield> </datafield> <datafield tag="542" ind1=" " ind2=" "> <subfield code="l">open</subfield> </datafield> <datafield tag="260" ind1=" " ind2=" "> <subfield code="c">2023-01-30</subfield> </datafield> <datafield tag="909" ind1="C" ind2="O"> <subfield code="p">openaire</subfield> <subfield code="p">user-ecotip-arctic</subfield> <subfield code="o">oai:zenodo.org:7603091</subfield> </datafield> <datafield tag="100" ind1=" " ind2=" "> <subfield code="u">UiT The Arctic University of Norway</subfield> <subfield code="0">(orcid)0000-0002-9274-3084</subfield> <subfield code="a">Wiedmann, Ingrid</subfield> </datafield> <datafield tag="245" ind1=" " ind2=" "> <subfield code="a">The west Greenland shelf (64.7-70.6 °N) plankton community and downward carbon flux during summer – an Atlantic influenced ecosystem?</subfield> </datafield> <datafield tag="980" ind1=" " ind2=" "> <subfield code="a">user-ecotip-arctic</subfield> </datafield> <datafield tag="536" ind1=" " ind2=" "> <subfield code="c">869383</subfield> <subfield code="a">Arctic biodiversity change and its consequences: Assessing, monitoring and predicting the effects of ecosystem tipping cascades on marine ecosystem services and dependent human systems</subfield> </datafield> <datafield tag="540" ind1=" " ind2=" "> <subfield code="u">https://creativecommons.org/licenses/by/4.0/legalcode</subfield> <subfield code="a">Creative Commons Attribution 4.0 International</subfield> </datafield> <datafield tag="650" ind1="1" ind2="7"> <subfield code="a">cc-by</subfield> <subfield code="2">opendefinition.org</subfield> </datafield> <datafield tag="520" ind1=" " ind2=" "> <subfield code="a"><p>On the West Greenland Shelf (64.7-70.6 &deg;N), Atlantic derived water flows northwards. This water gradually cools and becomes fresher at the surface, while it mixes with cold Baffin Bay Polar Waters (BBPW) at depth. We conducted a field study in August 2021 and investigated potential effects of these lateral changes in the water masses on the pelagic system. In particular, we studied how it affects the concentration of nitrate, suspended chlorophyll a (Chl a) and particulate organic carbon (POC), as well as the downward flux of POC and the protist community. We investigate here how the plankton communities and the quality and quantity of the downward carbon flux is linked to different water masses on the West Greenland Shelf.<br> This helps to better understand how intensified Atlantic influence may change the system.</p></subfield> </datafield> <datafield tag="773" ind1=" " ind2=" "> <subfield code="n">doi</subfield> <subfield code="i">isVersionOf</subfield> <subfield code="a">10.5281/zenodo.7603090</subfield> </datafield> <datafield tag="024" ind1=" " ind2=" "> <subfield code="a">10.5281/zenodo.7603091</subfield> <subfield code="2">doi</subfield> </datafield> <datafield tag="980" ind1=" " ind2=" "> <subfield code="a">poster</subfield> </datafield> </record>
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