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contributor authorFOSTER, DONALD S.
date accessioned2017-06-09T15:56:07Z
date available2017-06-09T15:56:07Z
date copyright1958/03/01
date issued1958
identifier issn0027-0644
identifier otherams-56985.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197270
description abstractThe buoyancy equation is integrated to find the downward speed of a parcel of air that becomes cooler than its environment and sinks to the ground, such as a downdraft in a thunderstorm. This downdraft speed is related to a positive energy area on a thermodynamic diagram. From a sample of one hundred soundings taken just prior to thunderstorm occurrences a correlation coefficient of 0.50 is obtained for the computed downdraft and measured wind gusts. Taking the upper wind speed into account fails to improve significantly the correlation coefficient. A correlation coefficient of only 0.22 is obtained for the direction of the surface wind gust and the wind direction in the 700?500-mb. layer.
publisherAmerican Meteorological Society
titleTHUNDERSTORM GUSTS COMPARED WITH COMPUTED DOWNDRAFT SPEEDS
typeJournal Paper
journal volume86
journal issue3
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1958)086<0091:TGCWCD>2.0.CO;2
journal fristpage91
journal lastpage94
treeMonthly Weather Review:;1958:;volume( 086 ):;issue: 003
contenttypeFulltext


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