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contributor authorGeisler, J. E.
date accessioned2017-06-09T14:16:15Z
date available2017-06-09T14:16:15Z
date copyright1972/03/01
date issued1972
identifier issn0022-4928
identifier otherams-16118.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151866
description abstractA simple two-dimensional model is used to demonstrate the importance of the vertical distribution of latent heat release for the functioning of CISK, When the horizontal scale of the prescribed heat source in the model is small (100 km), substantial heating at low levels is required in order to bring the zone of boundary-layer convergence into coincidence with the heat source. This effect is much less important for a large-scale (1000 km) source. In addition, lowering the base of the heated region favors CISK by increasing the upward mass transport per unit of prescribed heat release.
publisherAmerican Meteorological Society
titleOn the Vertical Distribution of Latent Heat Release and the Mechanics of CISK
typeJournal Paper
journal volume29
journal issue2
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1972)029<0240:OTVDOL>2.0.CO;2
journal fristpage240
journal lastpage243
treeJournal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 002
contenttypeFulltext


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