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- W178538169 abstract "A study was made to determine the depth of the drainage driven flows initiated by nocturnal surface cooling. Three methods used to determine the depth of the drainage layer from vertical profiles of meteorological data wwere evaluated. These are a shift in wind direction, the top of the surface based inversion, and the velocity minimum above the surfac layer jet. For relatively simple slope sites good agreement was found among all three methods of depth determination. In Brush Creek, a well defined valley, all three methods also indicated the same depth of drainage flow. When there was no clear wind direction shift at this site, the depths determined from the velocity minimum and the surface inversion were in agreement. At the somewhat more complicated Corral Gulch site, measurements were made in a shallow gulch imbedded in an extensive sloping terrain feature. There we found good agreement between the shift in wind direction and the velocity minimum, but the top of the drainage layer as determined from the surface inversion was always greater. In the outflow of the Anderson Creek basin, an area where possible flow divergence existed due to the deterioration of confining terrain, there was more variation in themore » results of the three methods. Results of an analysis of vertical profiles which were amenable to the application of all three methods are discussed.« less" @default.
- W178538169 created "2016-06-24" @default.
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- W178538169 date "1983-01-01" @default.
- W178538169 modified "2023-09-27" @default.
- W178538169 title "Determining depths of drainage winds" @default.
- W178538169 hasPublicationYear "1983" @default.
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