A statistical study of the correlation between the surface and surface geostrophic winds in the Wilamette Valley
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 geostr...
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Language: | en_US |
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2012
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Online Access: | http://hdl.handle.net/1957/29501 |