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contributor authorHookings, G. A.
date accessioned2017-06-09T16:40:20Z
date available2017-06-09T16:40:20Z
date copyright1965/04/01
date issued1965
identifier issn0021-8952
identifier otherams-7194.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213889
description abstractA first quantitative estimate of the maintenance of a downdraft by the evaporation of precipitation is made for the steady state of a severe convective storm. Results are presented for a sufficiently wide range of drop size, liquid water content and relative humidity for the trends to be determined. It is confirmed that cooling by evaporation is most efficient if the drop radii are small, and that the most severe downdrafts are produced in air from the upper troposphere which is notably dry.
publisherAmerican Meteorological Society
titlePrecipitation-Maintained Downdrafts
typeJournal Paper
journal volume4
journal issue2
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1965)004<0190:PMD>2.0.CO;2
journal fristpage190
journal lastpage195
treeJournal of Applied Meteorology:;1965:;volume( 004 ):;issue: 002
contenttypeFulltext


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