Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Raphael Dussin"'
Autor:
Hemant Khatri, Stephen M. Griffies, Benjamin A. Storer, Michele Buzzicotti, Hussein Aluie, Maike Sonnewald, Raphael Dussin, Andrew Shao
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 16, Iss 6, Pp n/a-n/a (2024)
Abstract The climatological mean barotropic vorticity budget is analyzed to investigate the relative importance of surface wind stress, topography, planetary vorticity advection, and nonlinear advection in dynamical balances in a global ocean simulat
Externí odkaz:
https://doaj.org/article/dbc793163f4a4675b36fe8f130c51c0f
Autor:
Raphael Dussin
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 39:1717-1728
A novel method to adjust the precipitation produced by atmospheric reanalyses using observational constraints to force ocean models is described. The method allows the preservation of the qualities of the high-resolution and high-frequency output fro
Autor:
Hemant Khatri, Stephen M Griffies, Benjamin A Storer, Michele Buzzicotti, Hussein Aluie, Maike Sonnewald, Raphael Dussin, Andrew E. Shao
The climatological mean barotropic vorticity budget is analyzed to investigate the relative importance of surface wind stress, topography and nonlinear advection in dynamical balances in a global ocean simulation. In addition to a pronounced regional
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31341c87de304b79d5c85642e2acb274
https://doi.org/10.22541/essoar.168394747.71837050/v1
https://doi.org/10.22541/essoar.168394747.71837050/v1
Autor:
Lauren Moseley, Galen McKinley, Dustin Carroll, Raphael Dussin, Dimitris Menemenlis, An Nguyen
The subpolar North Atlantic (SPNA) transports surface-ocean properties deep into the interior via deep convection and is one of the most intense regions of air-sea gas exchange globally. Deep convection in the SPNA exports highly-oxygenated water mas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bef0779c63def3463afcbbb402b81f6d
https://doi.org/10.5194/egusphere-egu23-15366
https://doi.org/10.5194/egusphere-egu23-15366
Autor:
Nathalí Cordero-Quirós, Arthur J. Miller, Yunchun Pan, Lawrence Balitaan, Enrique Curchitser, Raphael Dussin
Publikováno v:
Ocean Dynamics. 72:21-36
Autor:
Michael A. Alexander, Muyin Wang, Elizabeth J. Drenkard, Alistair Adcroft, Kirstin K. Holsman, Charles A. Stock, Vincent S. Saba, Chan Joo Jang, Albert J. Hermann, Raphael Dussin, Emanuele Di Lorenzo, Momme Butenschön, Keith W. Dixon, Anne Britt Sandø, Kelly A. Kearney, Barbara A. Muhling, Matthew Harrison, Desiree Tommasi, Wei Cheng, Anne B. Hollowed, Jason Holt, Alan C. Haynie, Michael G. Jacox, Venkatramani Balaji, Mercedes Pozo Buil, Enrique N. Curchitser, Andrew C. Ross, Steven J. Bograd
Publikováno v:
ICES Journal of Marine Science. 78:1969-1987
Efforts to manage living marine resources (LMRs) under climate change need projections of future ocean conditions, yet most global climate models (GCMs) poorly represent critical coastal habitats. GCM utility for LMR applications will increase with h
Autor:
Charles A. Stock, David J. Hill, Seth L. Danielson, Brita Irving, Cristina Schultz, Scott C. Doney, Enrique N. Curchitser, Claudine Hauri, Kate Hedstrom, Raphael Dussin
Publikováno v:
Biogeosciences, Vol 17, Pp 3837-3857 (2020)
The coastal ecosystem of the Gulf of Alaska (GOA) is especially vulnerable to the effects of ocean acidification and climate change. Detection of these long-term trends requires a good understanding of the system’s natural state. The GOA is a highl
Autor:
Raphael Dussin, Charles A. Stock, L. Hahn-Woernle, Brian Powell, Tobias Friedrich, Enrique N. Curchitser
Publikováno v:
Journal of Geophysical Research: Oceans. 126
Publikováno v:
Journal of Geophysical Research: Oceans. 124:2969-2991
Autor:
Andrew D. Barton, Charles A. Stock, N. Van Oostende, Raphael Dussin, Enrique N. Curchitser, Bettie Ward, John P. Dunne
Publikováno v:
Progress in Oceanography. 168:232-247
The measured concentration of chlorophyll a in the surface ocean spans four orders of magnitude, from ∼0.01 mg m−3 in the oligotrophic gyres to >10 mg m−3 in coastal zones. Productive regions encompass only a small fraction of the global ocean