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dc.contributor.authorAnderson, Kenneth
dc.contributor.authorFrederickson, Paul
dc.contributor.authorTerrill, Eric
dc.date.accessioned2014-05-19T16:05:58Z
dc.date.available2014-05-19T16:05:58Z
dc.date.issued2003
dc.identifier.urihttp://hdl.handle.net/10945/41316
dc.description.abstractMicrowave and electro-optical signal propagation over a wind-roughened sea is strongly dependent on signal interaction with the sea surface, the mean profiles of pressure (P), humidity (Q), temperature (T), wind (U) and their turbulent fluctuations (p, q, t, u). Yet, within the marine surface layer, these mechanisms are not sufficiently understood nor has satisfactory data been taken to validate propagation models, especially under conditions of high seas, high winds, and large surface gradients of Q and T. To address this deficiency, the Rough Evaporation Duct (RED) experiment was designed to provide first data for validation of meteorological, microwave, and electro-optical (EO) models in the marine surface layer for rough surface conditions including the effects of surface waves.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.titleAir-sea interaction effects on microwave propagation over the sea during the rough evaporation duct (red) experimenten_US
dc.typeArticleen_US
dc.contributor.departmentMeteorology


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