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dc.contributor.authorCsanady, Gabriel T.  Concept link
dc.date.accessioned2017-07-14T17:33:14Z
dc.date.available2017-07-14T17:33:14Z
dc.date.issued1982-12
dc.identifier.urihttps://hdl.handle.net/1912/9104
dc.descriptionAuthor Note: The material of this report was presented ten years ago at a symposium, but on account of its speculative nature, remained unpublished. Several colleagues were, however, kind enough to quote it on occasion (e.g. Garrett, 1982) and some have requested copies. In order to make it more readily available, it has now been re-issued as a WHOI report. Paper presented at the Canadian Committee of Oceanography Symposium, Burlington, Ontario, May 4, 1972.en_US
dc.description.abstractA first order, linear analysis of thermocline upwelling shows that a quasigeostrophic baroclinic jet accompanies the upwelling. The secondary circulation induced in such a flow field in a meridional plane by turbulent friction is investigated. A double Ekman layer is found to form at the thermocline, of a few meters in thickness. The suction of this Ekman layer destroys the primary flow by the "spin-up" mechanism in a period of which the order of magnitude is tentatively estimated at 100 hrs. Thus the primary flow must be reestablished by successive, reasonably frequent wind-stress impulses to maintain a quasi-stationary upwelling. The lower side Ekman layer on the thermocline is fed from a free shear layer (turbulent "Stewartson layer") underneath the free surface -thermocline intersection, which thus becomes an upwelling zone. The width of the turbulent Stewartson layer is estimated to be the velocity difference divided by the Coriolis parameter, i.e. typically of the order of 1 km.en_US
dc.description.sponsorshipPrepared for NOAA, Great Lakes Environmental Research Laboratory, Ann Arbor, Michigan.en_US
dc.language.isoen_USen_US
dc.publisherWoods Hole Oceanographic Institutionen_US
dc.relation.ispartofseriesWHOI Technical Reportsen_US
dc.relation.ispartofseriesWHOI-82-52en_US
dc.subjectUpwellingen_US
dc.subjectThermoclinesen_US
dc.titleFrictional secondary circulation near an upwelled thermoclineen_US
dc.typeTechnical Reporten_US
dc.identifier.doi10.1575/1912/9104


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