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dc.contributor.advisorGlenn Flierl.en_US
dc.contributor.authorCampbell, Donald Alberten_US
dc.contributor.otherMassachusetts Institute of Technology. Dept. of Meteorology.en_US
dc.date.accessioned2010-02-09T16:29:26Z
dc.date.available2010-02-09T16:29:26Z
dc.date.copyright1980en_US
dc.date.issued1980en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/51416
dc.descriptionThesis (M.S.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1980.en_US
dc.descriptionMicrofiche copy available in Archives and Science.en_US
dc.descriptionBibliography: leaves 85-88.en_US
dc.description.statementofresponsibilityby Donald Albert Campbell.en_US
dc.format.extent88 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.subjectMeteorology.en_US
dc.subject.lcshOcean currents Mathematical modelsen_US
dc.subject.lcshOcean circulation Mathematical modelsen_US
dc.titleQuasi-geostrophic jet meanderingen_US
dc.typeThesisen_US
dc.description.degreeM.S.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Meteorologyen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.identifier.oclc07772091en_US


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