Spatial distribution of air-sea heat fluxes over the sub-polar North Atlantic Ocean

Moore, G. W. K., Renfrew, IA ORCID: https://orcid.org/0000-0001-9379-8215 and Pickart, R. S. (2012) Spatial distribution of air-sea heat fluxes over the sub-polar North Atlantic Ocean. Geophysical Research Letters, 39 (18). ISSN 1944-8007

[thumbnail of moore_etal_subpolar_fluxes_2012GL053097_GRL_2012.pdf]
Preview
PDF (moore_etal_subpolar_fluxes_2012GL053097_GRL_2012.pdf) - Published Version
Download (2MB) | Preview

Abstract

On 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.

Item Type: Article
Faculty \ School: Faculty of Science > School of Environmental Sciences
University of East Anglia Research Groups/Centres > Theme - ClimateUEA
UEA Research Groups: Faculty of Science > Research Groups > Marine and Atmospheric Sciences (former - to 2017)
Faculty of Science > Research Groups > Meteorology, Oceanography and Climate Dynamics (former - to 2017)
Faculty of Science > Research Groups > Climate, Ocean and Atmospheric Sciences (former - to 2017)
Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences
Depositing User: Users 2731 not found.
Date Deposited: 20 Mar 2013 14:39
Last Modified: 20 Mar 2023 10:31
URI: https://ueaeprints.uea.ac.uk/id/eprint/41955
DOI: 10.1029/2012GL053097

Actions (login required)

View Item View Item