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contributor authorHaman, K. E.
date accessioned2017-06-09T16:02:16Z
date available2017-06-09T16:02:16Z
date copyright1978/11/01
date issued1978
identifier issn0027-0644
identifier otherams-59397.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4199950
description abstractFrom the hypothesis that a quasi-steady convective storm adjusts its internal flow to the ambient wind field, the velocity of the storm motion can be calculated by means of the Bernoulli equation. This velocity may be fairly dependent on the process of formation and discharge of precipitation.
publisherAmerican Meteorological Society
titleOn the Motion of a Three-Dimensional Quasi-Steady Convective Storm in Shear
typeJournal Paper
journal volume106
journal issue11
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1978)106<1622:OTMOAT>2.0.CO;2
journal fristpage1622
journal lastpage1627
treeMonthly Weather Review:;1978:;volume( 106 ):;issue: 011
contenttypeFulltext


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