Midlatitude wind stress–sea surface temperature coupling in the vicinity of oceanic fronts

dc.contributor.author Spall, Michael A.
dc.date.accessioned 2010-11-24T14:49:34Z
dc.date.available 2010-11-24T14:49:34Z
dc.date.issued 2007-08-01
dc.description Author Posting. © American Meteorological Society, 2007. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Climate 20 (2007): 3785–3801, doi:10.1175/JCLI4234.1 en_US
dc.description.abstract The influences of strong gradients in sea surface temperature on near-surface cross-front winds are explored in a series of idealized numerical modeling experiments. The atmospheric model is the Naval Research Laboratory Coupled Ocean–Atmosphere Mesoscale Prediction System (COAMPS) model, which is fully coupled to the Regional Ocean Modeling System (ROMS) ocean model. A series of idealized, two-dimensional model calculations is carried out in which the wind blows from the warm-to-cold side or the cold-to-warm side of an initially prescribed ocean front. The evolution of the near-surface winds, boundary layer, and thermal structure is described, and the balances in the momentum equation are diagnosed. The changes in surface winds across the front are consistent with previous models and observations, showing a strong positive correlation with the sea surface temperature and boundary layer thickness. The coupling arises mainly as a result of changes in the flux Richardson number across the front, and the strength of the coupling coefficient grows quadratically with the strength of the cross-front geostrophic wind. The acceleration of the winds over warm water results primarily from the rapid change in turbulent mixing and the resulting unbalanced Coriolis force in the vicinity of the front. Much of the loss/gain of momentum perpendicular to the front in the upper and lower boundary layer results from acceleration/deceleration of the flow parallel to the front via the Coriolis term. This mechanism is different from the previously suggested processes of downward mixing of momentum and adjustment to the horizontal pressure gradient, and is active for flows off the equator with sufficiently strong winds. Although the main focus of this work is on the midlatitude, strong wind regime, calculations at low latitudes and with weak winds show that the pressure gradient and turbulent mixing terms dominate the cross-front momentum budget, consistent with previous work. en_US
dc.description.sponsorship This work was supported by the Office of Naval Research Grant N00014-05-1-0300. en_US
dc.format.mimetype application/pdf
dc.identifier.citation Journal of Climate 20 (2007): 3785–3801 en_US
dc.identifier.doi 10.1175/JCLI4234.1
dc.identifier.uri https://hdl.handle.net/1912/4119
dc.language.iso en_US en_US
dc.publisher American Meteorological Society en_US
dc.relation.uri https://doi.org/10.1175/JCLI4234.1
dc.subject Fronts en_US
dc.subject Sea surface temperature en_US
dc.subject Wind stress en_US
dc.subject Coupled models en_US
dc.subject Boundary layer en_US
dc.title Midlatitude wind stress–sea surface temperature coupling in the vicinity of oceanic fronts en_US
dc.type Article en_US
dspace.entity.type Publication
relation.isAuthorOfPublication daaf5cc7-61e5-4a81-8b45-188e9160ebcb
relation.isAuthorOfPublication.latestForDiscovery daaf5cc7-61e5-4a81-8b45-188e9160ebcb
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