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dc.contributor.authorMiller, Douglas K.
dc.contributor.authorNuss, Wendell A.
dc.contributor.authorCross, Patrick S.
dc.date.accessioned2015-01-20T20:11:21Z
dc.date.available2015-01-20T20:11:21Z
dc.date.issued2003-08-05
dc.identifier.urihttp://hdl.handle.net/10945/44349
dc.descriptionFifth Conference on Coastal Atmospheric and Oceanic Prediction and Processes, August 5-8, 2003en_US
dc.description.abstractA low-level core of high wind speeds aligned along the U.S. West Coast, known as the coastal jet, is a persistent feature during the summer months. The seasonal preference for such a feature is a function of several conditions; warm temperatures inland, cool air offshore maintained by coastal upwelling, and a capping inversion at the top of the marine boundary layer forced by subsidence associated with the eastern Pacific sub-tropical high.en_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.en_US
dc.titleSensitivity of coastal jet structure to coastal topographyen_US
dc.typeArticleen_US
dc.contributor.departmentMeteorology


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