Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Karin Margretha H. Larsen"'
Publikováno v:
Frontiers in Marine Science, Vol 9 (2022)
Marine ecosystem dynamics can vary on timescales ranging from months to centuries, but many observational data are limited to just a few decades. The bivalve Arctica islandica may live up to five centuries depositing annual growth increments in its s
Externí odkaz:
https://doaj.org/article/8f7982a52d9f48efb3c59abeb60e2822
Autor:
Øystein Skagseth, Cecilie Broms, Kjell Gundersen, Hjálmar Hátún, Inga Kristiansen, Karin Margretha H. Larsen, Kjell Arne Mork, Hildur Petursdottir, Henrik Søiland
Publikováno v:
Frontiers in Marine Science, Vol 9 (2022)
The ocean climate of the southern Norwegian Sea - the Norwegian Basin - is largely set by the relative amount of Atlantic Water in the eastern and Arctic Water in the western region. Here we utilized hydrographic data from repeated sections, together
Externí odkaz:
https://doaj.org/article/85d277d118f84090974b55a922a35299
Autor:
Stefanie Semper, Robert S. Pickart, Kjetil Våge, Karin Margretha H. Larsen, Hjálmar Hátún, Bogi Hansen
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-10 (2020)
Dense water from the Nordic Seas sustains the Atlantic Meridional Overturning Circulation, yet the upstream pathways are not fully known. Here, the authors provide evidence of a deep current between Iceland and the Faroe Islands, which supplies 50% o
Externí odkaz:
https://doaj.org/article/170c0fd928fc4c9e87e061a2d5cdd78a
Autor:
Léon Chafik, Hjálmar Hátún, Joakim Kjellsson, Karin Margretha H. Larsen, Thomas Rossby, Barbara Berx
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-10 (2020)
The authors show that overflow waters flowing toward the Faroe Bank Channel can take a previously unidentified path to the Faroe-Shetland Channel where it joins an unrecognized deep-reaching jet located along its eastern rather than its western bound
Externí odkaz:
https://doaj.org/article/b0b36a5db10a4508b436b7a47d6d2837
Autor:
N. Penny Holliday, Manfred Bersch, Barbara Berx, Léon Chafik, Stuart Cunningham, Cristian Florindo-López, Hjálmar Hátún, William Johns, Simon A. Josey, Karin Margretha H. Larsen, Sandrine Mulet, Marilena Oltmanns, Gilles Reverdin, Tom Rossby, Virginie Thierry, Hedinn Valdimarsson, Igor Yashayaev
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-15 (2020)
The Atlantic Ocean overturning circulation is important to the global climate system. Here the authors show that eastern subpolar North Atlantic underwent extreme freshening during 2012 to 2016, with a magnitude never seen before in 120 years of surf
Externí odkaz:
https://doaj.org/article/8bfa1e0bf16a4417916ee3992950ed5b
Autor:
Boris Cisewski, Hjálmar Hátún, Inga Kristiansen, Bogi Hansen, Karin Margretha H. Larsen, Sólvá Káradóttir Eliasen, Jan Arge Jacobsen
Publikováno v:
Frontiers in Marine Science, Vol 7 (2021)
Records of backscatter and vertical velocity obtained from moored Acoustic Doppler Current Profilers (ADCP) enabled new insights into the dynamics of deep scattering layers (DSLs) and diel vertical migration (DVM) of mesopelagic biomass between these
Externí odkaz:
https://doaj.org/article/ade3c0551cad4822a7c3672308a7a06c
Autor:
Igor M. Belkin, Stefano Aliani, Matthew B. Alkire, Thomas H. Badewien, Maristella Berta, Gloria Silvana Durán Gómez, Sólvá Káradóttir Eliasen, Jüri Elken, Annalisa Griffa, Nicolas Gruber, Céline Guéguen, Hjálmar Hátún, Ramu Karri, Piotr Kowalczuk, Karin Margretha H. Larsen, Irina Marinov, Moritz Mathis, Jens Meyerjürgens, Anne Molcard, Takeyoshi Nagai, Tamay M. Özgökmen, Jaime B. Palter, Igor Polyakov, Robert Rember, Marcel Ricker, Jorge L. Sarmiento, Emil V. Stanev, Giuseppe Suaria, Ülo Suursaar, Shin Takahashi, Shinsuke Tanabe, Qin-Sheng Wei, Enrico Zambianchi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3b689d8184b26b1f12bad0dcdb5b2125
https://doi.org/10.1007/698_2022_894
https://doi.org/10.1007/698_2022_894
Publikováno v:
Frontiers in Marine Science, Vol 8 (2021)
The Norwegian Sea gyre (NSG) is a large body of Arctic intermediate water and deep dense overflow waters, which circulate counterclockwise within the Norwegian Sea. Argo float trajectories presented in this study suggest that the NSG attains its stro
Autor:
Karin Margretha H. Larsen, Steffen M. Olsen, Sólveig Rósa Ólafsdóttir, Bogi Hansen, Steingrímur Jónsson, Andreas Macrander, Hjálmar Hátún, William E. Johns, N. Penny Holliday
Outflows of low-salinity waters from the Arctic to the upper layers of the subpolar North Atlantic (SPNA) are central in redistributing freshwater from river runoff, melting sea ice, and precipitation. They act to reduce shallow, as well as deep, con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::132ef39550434b1cbb825899e3cff92e
https://os.copernicus.org/preprints/os-2021-14/
https://os.copernicus.org/preprints/os-2021-14/