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dc.contributor.advisorPauline M. Austin.en_US
dc.contributor.authorOmotoso, Elias Akanbien_US
dc.date.accessioned2005-09-26T17:56:15Z
dc.date.available2005-09-26T17:56:15Z
dc.date.issued1967en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/28001
dc.descriptionMassachusetts Institute of Technology. Dept. of Meteorology. Thesis. 1967. M.S.en_US
dc.descriptionBibliography: leaves 68-69.en_US
dc.format.extent[7], 69 leavesen_US
dc.format.extent3391467 bytes
dc.format.extent3399395 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypeapplication/pdf
dc.language.isoen_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/1721.1/7582
dc.subjectMeteorologyen_US
dc.titleDevelopment of the more intense storms in a well organized squall line.en_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.oclc25778394en_US


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