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111	Buoy and satellite observation of wind induced surface heat exchange in the intraseasonal oscillation over West Pacific and Indian Ocean / Araligidad, Nilesh. January 1900 (has links) Thesis (M.S.)--Oregon State University, 2008. / Printout. Includes bibliographical references (leaves 77-83). Also available on the World Wide Web.
112	Cyclogenesis Near the Adélie Coast and Influence of the Low-level Wind Regime Steinhoff, Daniel Frederick 19 March 2008 (has links) No description available. Atmosphere Antarctica cyclones mesoscale katabatic winds barrier winds
113	Binary stars and mass loss Tout, Christopher Adam January 1989 (has links) No description available. 523.01 Mass loss in stellar winds
114	A statistical study of the correlation between the surface and surface geostrophic winds in the Wilamette Valley Andrews, Leta 23 October 1974 (has links) Relationships among the surface wind, horizontal synoptic-scale pressure gradient and topography are studied in the Willamette Valley in western Oregon. Terrain features alter the standard surface wind-pressure gradient relationship such that the angle between the surface wind and the surface geostrophic wind is most frequently 60°. In winter the surface flow is predominantly southerly and surface geostrophic flow varies from southerly to westerly. Little diurnal change occurs in the average surface wind, the average surface geostrophic wind and their relationship with each other because the air in the valley is generally stably stratified throughout the day. Partially in response to the northward extension of the subtropical anticyclone summertime surface winds and surface geostrophic winds are northerly, except during afternoon episodes of marine air invasion when surface winds are westerly. The pressure gradient is 88% less intense in summer but the ratio of the magnitudes of the surface wind and surface geostrophic wind, R, is 125% greater than in winter. However, a sharp summertime morning maximum in R of -0.67 is diminished by early afternoon as differential surface heating establishes a strong afternoon pressure gradient. When the surface geostrophic wind vector is cross-valley, the surface wind is still most frequently parallel to the valley and the surface geostrophic wind speed is largest and most variable. Because of the importance of terrain and meso-scale events, little correlation between the surface winds and synoptic-scale pressure gradient is found. / Graduation date: 1975
115	The sea breeze of Northwest Oregon and its influence on forestry operations Lowry, William P. 10 May 1962 (has links) Graduation date: 1962 Sea air Winds Forest influences
116	Characteristics of monsoon and typhoon winds in Hong Kong from an engineering viewpoint. Ko, King-lim, Pius. January 1972 (has links) Thesis (Ph. D.)--University of Hong Kong, 1972. / Mimeographed.
117	The application of the theory of extremes to the estimation of design wind speeds. Lun, Chi Leung, Kenneth. January 1970 (has links) Thesis--M. Sc. (Eng.), University of Hong Kong. / Mimeographed. Wind-pressure. Winds Structural design.
118	Theory of air velocity measurement by dual-frequency Doppler lidar Eberhard, Wynn Lowell, 1944- January 1976 (has links) No description available. Laser Doppler velocimeter. Winds -- Measurement.
119	Adjustment of regional wind forecasts to the topography Allard, Hubert January 1974 (has links) No description available. Numerical weather forecasting. Winds -- Measurement.
120	Studies of the lower atmosphere with a VHF wind profiler / by David J. Low. Low, David J. (David John), 1969- January 1996 (has links) Bibliography: p. 249-267. / xxiv, 267 p., [1] leaf of plates : ill. ; 30 cm. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (Ph.D.)--University of Adelaide, Dept. of Physics and Mathematical Physics, 1996 551.518 21 Winds Measurement. Troposphere.

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