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Parameterization of convection in a rotating stratified ocean : comparison of numerical and laboratory experiments with theory

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dc.contributor.author Hufford, Gwyneth E.
dc.date.accessioned 2012-11-15T19:56:51Z
dc.date.available 2012-11-15T19:56:51Z
dc.date.issued 1995-02
dc.identifier.uri http://hdl.handle.net/1912/5557
dc.description Submitted in partial fulfillment of the requirements for the degree of Master of Science at the Massachusetts Institute of Technology and Woods Hole Oceanographic Institution February 1995 en_US
dc.description.abstract Laboratory and numerical experiments are carried out in a parameter regime relevant to open-ocean deep convection. We consider the case of convection in a rotating stratified ocean of finite depth. Convection is induced from the surface by extracting buoyancy over a circular area. The external parameters are buoyancy forcing of strength Bo applied over a circular area of radius Rs, the rotation rate is measured by f, ambient stratification N and finite depth H. Theoretical scaling predictions are derived to describe the length and velocity scales of the convective chimney as it adjusts under gravity and rotation, and breaks up through baroclinic instability. The scales of interest include the number (M), size (leddy) and strength (Urim) of the baroclinic eddies formed. Also of interest are the final depth of penetration of the convective mixed layer (dfinal) and the final volume of convectively produced water (Vfinal). These scales are tested against the laboratory and numerical experiments and found to be appropriate. We show that for this idealized problem dfinal depends only on the size and strength of the forcing and t he ambient stratification encountered by the convection event; it does not depend explicitly on rotation. The volume of convectively modified water produced continues to increase as long as forcing continues, but the rate of production depends again only on the size and strength of the forcing and on the ambient stratification. The implications of the work to deep water formation in the Labrador Sea and elsewhere are discussed. Finally, the study has relevance to the role and representation of baroclinic eddies in large-scale circulation of the ocean. en_US
dc.description.sponsorship This research was funded by John Marshall on Office of Naval Research (ONR) contract N00014-92-J-1567. en_US
dc.format.mimetype application/pdf
dc.language.iso en_US en_US
dc.publisher Massachusetts Institute of Technology and Woods Hole Oceanographic Institution en_US
dc.relation.ispartofseries WHOI Theses en_US
dc.subject Density currents en_US
dc.title Parameterization of convection in a rotating stratified ocean : comparison of numerical and laboratory experiments with theory en_US
dc.type Thesis en_US
dc.identifier.doi 10.1575/1912/5557


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