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dc.contributor.authorMoore, G. W. K.
dc.contributor.authorRenfrew, Ian A.
dc.contributor.authorPickart, Robert S.
dc.date.accessioned2012-11-07T20:46:35Z
dc.date.available2014-10-22T08:57:23Z
dc.date.issued2012-09-27
dc.identifier.citationGeophysical Research Letters 39 (2012): L18806en_US
dc.identifier.urihttp://hdl.handle.net/1912/5523
dc.descriptionAuthor Posting. © American Geophysical Union, 2012. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 39 (2012): L18806, doi:10.1029/2012GL053097.en_US
dc.description.abstractOn a variety of spatial and temporal scales, the energy transferred by air-sea heat and moisture fluxes plays an important role in both atmospheric and oceanic circulations. This is particularly true in the sub-polar North Atlantic Ocean, where these fluxes drive water-mass transformations that are an integral component of the Atlantic Meridional Overturning Circulation (AMOC). Here we use the ECMWF Interim Reanalysis to provide a high-resolution view of the spatial structure of the air-sea turbulent heat fluxes over the sub-polar North Atlantic Ocean. As has been previously recognized, the Labrador and Greenland Seas are areas where these fluxes are large during the winter months. Our particular focus is on the Iceland Sea region where, despite the fact that water-mass transformation occurs, the winter-time air-sea heat fluxes are smaller than anywhere else in the sub-polar domain. We attribute this minimum to a saddle point in the sea-level pressure field, that results in a reduction in mean surface wind speed, as well as colder sea surface temperatures associated with the regional ocean circulation. The magnitude of the heat fluxes in this region are modulated by the relative strength of the Icelandic and Lofoten Lows, and this leads to periods of ocean cooling and even ocean warming when, intriguingly, the sensible and latent heat fluxes are of opposite sign. This suggests that the air-sea forcing in this area has large-scale impacts for climate, and that even modest shifts in the atmospheric circulation could potentially impact the AMOC.en_US
dc.description.sponsorshipGWKM was supported by the Natural Science and Engineering Research Council of Canada. IAR was funded in part by NCAS (the National Centre for Atmospheric Sciences) and by NERC grant NE/I005293/1. RSP was funded by grant OCE-0959381 fromthe US National Science Foundation.en_US
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dc.language.isoen_USen_US
dc.publisherAmerican Geophysical Unionen_US
dc.relation.urihttps://doi.org/10.1029/2012GL053097
dc.subjectAir-sea interactionen_US
dc.subjectClimate variabilityen_US
dc.subjectWater mass transformationen_US
dc.titleSpatial distribution of air-sea heat fluxes over the sub-polar North Atlantic Oceanen_US
dc.typeArticleen_US
dc.description.embargo2013-03-27en_US
dc.identifier.doi10.1029/2012GL053097


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