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dc.contributor.advisorPaola Malanotte-Rizzoli.en_US
dc.contributor.authorVennell, M. Rossen_US
dc.contributor.otherMassachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences.en_US
dc.date.accessioned2010-09-01T13:25:29Z
dc.date.available2010-09-01T13:25:29Z
dc.date.copyright1988en_US
dc.date.issued1988en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/57927
dc.descriptionThesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmosphere and Planetary Sciences, 1988.en_US
dc.descriptionIncludes bibliographical references.en_US
dc.description.statementofresponsibilityby M. Ross Vennell.en_US
dc.format.extent198 leavesen_US
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsM.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582en_US
dc.subjectEarth, Atmospheric, and Planetary Sciences.en_US
dc.titleThe influence of a steady baroclinic deep ocean on the shelfen_US
dc.typeThesisen_US
dc.description.degreePh.D.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.identifier.oclc20205569en_US


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