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dc.contributor.authorLeetmaa, Ants  Concept link
dc.contributor.authorBunker, Andrew F.  Concept link
dc.date.accessioned2018-10-02T18:36:57Z
dc.date.available2018-10-02T18:36:57Z
dc.date.issued1978-08
dc.identifier.urihttps://hdl.handle.net/1912/10613
dc.descriptionAlso published as: Journal of Marine Research, Volwne 36, 3, 1978, pp. 311-322.en_US
dc.description.abstractFrom the wind stress computation of Bunker (1976) for the North Atlantic, the annual mean and seasonal vertical velocities which result from convergences in the Ekman Layers are computed. Charts of the geostrophic and total transport (geostrophic plus Ekman) are constructed using the Sverdrup relationship. Of particular interest are an intense current leaving the coast at the point where the Gulf Stream separates and a cyclonic gyre north of the Stream in this area. Good agreement exists between the computed features of the large scale circulation patterns and the observed ones. Close correspondence exists between the predicted and observed paths of the Gulf Stream; separation from the coast occurs at the maxima in the wind stress.en_US
dc.description.sponsorshipPrepared for the Office of Naval Research under Contract N00014-74-C-0262; NR 083-004.en_US
dc.language.isoen_USen_US
dc.publisherWoods Hole Oceanographic Institutionen_US
dc.relation.ispartofseriesWHOI Technical Reportsen_US
dc.relation.ispartofseriesWHOI-78-53en_US
dc.subjectWindsen_US
dc.subjectOcean-atmosphere interactionen_US
dc.titleUpdated charts of the mean annual wind stress, convergences in the Ekman layers, and Sverdrup transports in the North Atlanticen_US
dc.typeTechnical Reporten_US
dc.identifier.doi10.1575/1912/10613


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