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contributor authorHering, Wayne S.
contributor authorBorden, Thomas R.
date accessioned2017-06-09T14:12:49Z
date available2017-06-09T14:12:49Z
date copyright1962/01/01
date issued1962
identifier issn0022-4928
identifier otherams-14816.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150419
description abstractResults of a brief descriptive study of the diurnal wind variation over the central United States are presented. Six-hourly rawin observations for July, 1958, at Fort Worth and Shreveport were used to compute the average wind oscillation at selected levels up to 25 km. Two prominent diurnal wind regimes were observed above the boundary layer oscillation centered at 0.6 km. Maximum amplitudes of the upper-level oscillations were observed at about 5 km and 12 km. Limited analysis of rawin data from other stations indicates the observed diurnal wind system extended from the Appalachian Mountains westward to the Rocky Mountain area.
publisherAmerican Meteorological Society
titleDIURNAL VARIATIONS IN THE SUMMER WIND FIELD OVER THE CENTRAL UNITED STATES
typeJournal Paper
journal volume19
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1962)019<0081:DVITSW>2.0.CO;2
journal fristpage81
journal lastpage86
treeJournal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 001
contenttypeFulltext


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