Zobrazeno 1 - 10
of 1 599
pro vyhledávání: '"H Valdimarsson"'
Autor:
S. Østerhus, R. Woodgate, H. Valdimarsson, B. Turrell, L. de Steur, D. Quadfasel, S. M. Olsen, M. Moritz, C. M. Lee, K. M. H. Larsen, S. Jónsson, C. Johnson, K. Jochumsen, B. Hansen, B. Curry, S. Cunningham, B. Berx
Publikováno v:
Ocean Science, Vol 15, Pp 379-399 (2019)
The Arctic Mediterranean (AM) is the collective name for the Arctic Ocean, the Nordic Seas, and their adjacent shelf seas. Water enters into this region through the Bering Strait (Pacific inflow) and through the passages across the Greenland–Scotla
Externí odkaz:
https://doaj.org/article/69cd8ba8071d4d8aa4796fb19a849ab7
Autor:
G. Reverdin, N. Metzl, S. Olafsdottir, V. Racapé, T. Takahashi, M. Benetti, H. Valdimarsson, A. Benoit-Cattin, M. Danielsen, J. Fin, A. Naamar, D. Pierrot, K. Sullivan, F. Bringas, G. Goni
Publikováno v:
Earth System Science Data, Vol 10, Pp 1901-1924 (2018)
This paper presents the SURATLANT data set (SURveillance ATLANTique). It consists of individual data of temperature, salinity, parameters of the carbonate system, nutrients, and water stable isotopes (δ18O and δD) collected mostly from ships of
Externí odkaz:
https://doaj.org/article/6972557899b446449ef003d805741219
Autor:
G. Reverdin, H. Valdimarsson, G. Alory, D. Diverres, F. Bringas, G. Goni, L. Heilmann, L. Chafik, T. Szekely, A. R. Friedman
Publikováno v:
Earth System Science Data, Vol 10, Pp 1403-1415 (2018)
We present a binned product of sea surface temperature, sea surface salinity, and sea surface density data in the North Atlantic subpolar gyre from 1993 to 2017 that resolves seasonal variability along specific ship routes (https://doi.org/10.6096
Externí odkaz:
https://doaj.org/article/9f342fad31db4442b1fa8e50f58978b4
Autor:
Bernard F. Erlanger
Publikováno v:
Immunology Today. 15:248
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef598441f2795bf26cdfe1312b604ac7
https://doi.org/10.1016/0167-5699(94)90253-4
https://doi.org/10.1016/0167-5699(94)90253-4
Biased thermohaline exchanges with the Arctic across the Iceland–Faroe Ridge in ocean climate models
Publikováno v:
Ocean Science, Vol 12, Iss 2, Pp 545-560 (2016)
The northern limb of the Atlantic thermohaline circulation and its transport of heat and salt towards the Arctic strongly modulate the climate of the Northern Hemisphere. The presence of warm surface waters prevents ice formation in parts of the Arct
Externí odkaz:
https://doaj.org/article/68e9f5d18e584c09a7a0e64c90be8009
Akademický článek
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Publikováno v:
Ocean Science, Vol 9, Iss 5, Pp 931-955 (2013)
The three-dimensional flow, temperature and salinity fields of the North Atlantic, including the Arctic Ocean, covering the time period 1992 to 2006 are simulated with the numerical ocean model CODE. The simulation reveals several new insights and pr
Externí odkaz:
https://doaj.org/article/d593beb5aae94b61846aa8f1ab267dc7
Publikováno v:
Journal of Geophysical Research: Oceans. 124:7947-7961
The Denmark Strait overflow is the major export route of dense water from the Arctic Mediterranean into the North Atlantic. At the Strait's shallow sill, the overflow is a bottom-intensified cold and dense plume, bound to the east by a thermal front
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::530b80c75921cdfe341c122a8427be8a
https://doi.org/10.1029/2019jc015273
https://doi.org/10.1029/2019jc015273
Autor:
S. Østerhus, R. Woodgate, H. Valdimarsson, B. Turrell, L. de Steur, D. Quadfasel, S. M. Olsen, M. Moritz, C. M. Lee, K. M. H. Larsen, S. Jónsson, C. Johnson, K. Jochumsen, B. Hansen, B. Curry, S. Cunningham, B. Berx
Publikováno v:
Ocean Science
Ocean Science, Vol 15, Pp 379-399 (2019)
Ocean Science, Vol 15, Pp 379-399 (2019)
The Arctic Mediterranean (AM) is the collective name for the Arctic Ocean, the Nordic Seas, and their adjacent shelf seas. Water enters into this region through the Bering Strait (Pacific inflow) and through the passages across the Greenland–Scotla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0ddb69cc40f2f5ee3e92c4e7d5a8c135
https://doi.org/10.5194/os-2018-114
https://doi.org/10.5194/os-2018-114
