Zobrazeno 1 - 5
of 5
pro vyhledávání: '"K. M. Assmann"'
Autor:
J. Clement Kinney, K. M. Assmann, W. Maslowski, G. Björk, M. Jakobsson, S. Jutterström, Y. J. Lee, R. Osinski, I. Semiletov, A. Ulfsbo, I. Wåhlström, L. G. Anderson
Publikováno v:
Ocean Science, Vol 18, Pp 29-49 (2022)
Substantial amounts of nutrients and carbon enter the Arctic Ocean from the Pacific Ocean through the Bering Strait, distributed over three main pathways. Water with low salinities and nutrient concentrations takes an eastern route along the Alaskan
Externí odkaz:
https://doaj.org/article/1783672dd6424b1eaa520fef536a74d8
Autor:
W. Wei, D. D. Blankenship, J. S. Greenbaum, N. Gourmelen, C. F. Dow, T. G. Richter, C. A. Greene, D. A. Young, S. Lee, T.-W. Kim, W. S. Lee, K. M. Assmann
Publikováno v:
The Cryosphere, Vol 14, Pp 1399-1408 (2020)
Antarctica's Getz Ice Shelf has been rapidly thinning in recent years, producing more meltwater than any other ice shelf in the world. The influx of fresh water is known to substantially influence ocean circulation and biological productivity, but re
Externí odkaz:
https://doaj.org/article/735f8ce5320945fa8ebdcfbdfc34c2f7
Autor:
J. Schwinger, N. Goris, J. F. Tjiputra, I. Kriest, M. Bentsen, I. Bethke, M. Ilicak, K. M. Assmann, C. Heinze
Publikováno v:
Geoscientific Model Development, Vol 9, Iss 8, Pp 2589-2622 (2016)
Idealised and hindcast simulations performed with the stand-alone ocean carbon-cycle configuration of the Norwegian Earth System Model (NorESM-OC) are described and evaluated. We present simulation results of three different model configurations (two
Externí odkaz:
https://doaj.org/article/a211c41137a6457cbb4a3bdf05aec252
Publikováno v:
Geoscientific Model Development, Vol 3, Iss 1, Pp 143-167 (2010)
The carbon cycle is a major forcing component in the global climate system. Modelling studies, aiming to explain recent and past climatic changes and to project future ones, increasingly include the interaction between the physical and biogeochemical
Externí odkaz:
https://doaj.org/article/1cb32f33df424c0887680413ee0e81b6
Autor:
A K, Wåhlin, N, Steiger, E, Darelius, K M, Assmann, M S, Glessmer, H K, Ha, L, Herraiz-Borreguero, C, Heuzé, A, Jenkins, T W, Kim, A K, Mazur, J, Sommeria, S, Viboud
Publikováno v:
Nature. 578(7796)
Mass loss from the Antarctic Ice Sheet to the ocean has increased in recent decades, largely because the thinning of its floating ice shelves has allowed the outflow of grounded ice to accelerate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::7a21f0de8005ce2d929c6bcab5286f9f
https://pubmed.ncbi.nlm.nih.gov/32103192
https://pubmed.ncbi.nlm.nih.gov/32103192