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Profile functions for the diabatic surface layer a 'New Approach' /McCalla, Carl. January 1980 (has links)
Thesis (M.S.)--University of Wisconsin--Madison. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 73-77).
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Analysis of the observed velocity and vorticity fields around a vertical cylindrical obstaclMiller, Norman Leslie. January 1981 (has links)
Thesis (M.S.)--University of Wisconsin--Madison, 1981. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 52-53).
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A technique for utilizing satellite derived geostrophic windsKalb, Michael Wayne. January 1979 (has links)
Thesis (M.S.)--University of Wisconsin--Madison. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 72-73).
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Investigations of the modification of wind profiles by artificially controlled surface roughnessKutzbach, John E. January 1961 (has links)
Thesis (M.S.)--University of Wisconsin--Madison, 1961. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves [29-30]).
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Monitory and validation of the wind characteristics at the Stonecutters Bridge site /Au, Man Kai. January 2007 (has links)
Thesis (M.Phil.)--Hong Kong University of Science and Technology, 2007. / Includes bibliographical references (leaves 187-189). Also available in electronic version.
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Forcing and structure of the 22-25 June 2006 coastally trapped wind reversal using aircraft observations and numerical simulationsRahn, David. January 2008 (has links)
Thesis (Ph.D.)--University of Wyoming, 2008. / Title from PDF title page (viewed on Apr. 1, 2010). Includes bibliographical references (p. 96-99).
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Resolving the diurnal and synoptic variance of scatterometer vector wind observationsLombardi, Khara C. Bourassa, Mark A. January 2004 (has links)
Thesis (M.S.)--Florida State University, 2004. / Advisor: Dr. Mark Bourassa, Florida State University, College of Arts and Sciences, Dept. of Meteorology. Title and description from dissertation home page (Jan. 20, 2005). Includes bibliographical references.
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The feasibility of sodar wind profile measurements from an oceanographic buoyBerg, Allison M. January 2006 (has links) (PDF)
Thesis (M.S.)--Massachusetts Institute of Technology at Woods Hole Oceanographic Institution, 2006. / "September 2006." Description based on title screen as viewed on June 8, 2010. DTIC Descriptor(s): Doppler Radar, Wind Velocity, Sound Ranging, Doppler Sonar, Buoys, Measurement, Motion, Oceanographic Equipment, Theses DTIC Identifier(s): Doppler Sodar, Sodar (Sound Detection and Ranging), ASIS Includes bibliographical references (leaf 75). Also available in print.
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The feasibility of sodar wind profile measurements from an oceanographic buoy /Berg, Allison M. January 1900 (has links)
Thesis (M.S.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology; and the Woods Hole Oceanographic Institution), 2006. / Bibliography: p. 75.
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Ocean mixed layer response to gap wind scenariosKonstantinou, Nikolaos 12 1900 (has links)
This study focuses on understanding the oceanic response to gap outflow and the air-sea interaction precesses during the gap wind event between 26 and 28 February 2004 over the Gulf of Tehuantepec, Mexico. The U.S. Navy's Coupled Ocean Atmospheric Mesoscale Prediction Systems (COAMPS) and NPS Ocean Mixed Layer (OML) model was used to simulate the gap wind event and the temporal/spatial evolution of ocean response. Satellites, coincident in situ aircraft and AXBTs measurements of the sea surface temperature and the water temperature profiles collected during the Gulf of Tehuantepec Experiment (GOTEX) were used to define model initial conditions and aid the analysis of model results. Results for the OML simulations suggest measurable SST evolution as a result of the enhanced upper ocean mixing along the jet axes. Model sensitivity tests show the dominant effects of surface heat flux in generating upper ocean mixing while mechanical forcing by the strong wind of the gap outflow has secondary effects. Sensitivity tests also suggest that the thermocline structure is the most important factor in determing the magnitude of the ocean response while variations in SST are not sensitive to upwelling for a short time scale of several days. The study of COAMPS/OML simulations and satellite (SST) images confirms the existence of a secondary gap outflow source in the area.
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