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Abrupt cooling over the North Atlantic in modern climate models
Observations over the 20th century evidence no long-term warming in the subpolar North Atlantic (...
G Sgubin, D Swingedouw, SS Drijfhout | Status: accepted | Journal: Nature Communications | Volume: 8 | Year: 2017 | doi: https://doi.org/10.1038/ncomms14375
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Observation Representativeness Error
NWP models simulate the atmospheric state on a given model grid, thereby principally
limiting the...
GJ Marseille, A Stoffelen | Year: 2012
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Polar amplification in a coupled climate model with locked albedo
In recent years, a substantial reduction of the
sea ice in the Arctic has been observed. At the s...
RG Graversen, M Wang | Status: published | Journal: Clim. Dyn. | Volume: 33 | Year: 2009 | First page: 629 | Last page: 643 | doi: 10.1007/s00382-009-0535-6
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Boundary-layer model results for wind-sea growth
A numerical model of the boundary layer of the atmosphere above a gravity surface wave is rev...
G Burgers, VK Makin | Status: published | Journal: J. Phys. Oceanogr. | Volume: 23 | Year: 1993 | First page: 372 | Last page: 385
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On the air-sea coupling in the WAM wave model
Wind generates waves on the surface of the ocean. Modifications of the sea state influence the wi...
DF Doortmont, VK Makin | Year: 2000 | Pages: 55
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