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dc.contributor.advisorPeter B. Rhines.en_US
dc.contributor.authorYoung, William Royen_US
dc.contributor.otherMassachusetts Institute of Technology. Dept. of Meteorology.en_US
dc.date.accessioned2010-09-01T13:22:46Z
dc.date.available2010-09-01T13:22:46Z
dc.date.issued1981en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/57916
dc.descriptionThesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1981.en_US
dc.descriptionMicrofiche copy available in Archives and Science.en_US
dc.descriptionBibliography: leaves 210-215.en_US
dc.description.statementofresponsibilityby William Roy Young.en_US
dc.format.extenti, 215 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 circulation Mathematical modelsen_US
dc.subject.lcshOcean currents Mathematical modelsen_US
dc.subject.lcshRossby wavesen_US
dc.titleThe vertical structure of the wind-driven circulationen_US
dc.typeThesisen_US
dc.description.degreePh.D.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.oclc09193185en_US


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