A NOTE ON CUMULUS GROWTH IN A NONSATURATED ENVIRONMENTSource: Journal of Meteorology:;1948:;volume( 005 ):;issue: 003::page 103Author:Austin, James M.
DOI: 10.1175/1520-0469(1948)005<0103:ANOCGI>2.0.CO;2Publisher: American Meteorological Society
Abstract: On the basis of certain evidence it is concluded that mixing between the cumulus cloud and its environment affects the development of the cloud. It is shown that, for the case of mixing, the lapse rate of temperature within the cloud is greater than the moist-adiabatic rate and also that low relative humidities within the environment disfavor the cloud growth. A synoptic study supports the hypothesis that the forecast of convective showers should take into consideration the relative humidity above the convective condensation level.
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contributor author | Austin, James M. | |
date accessioned | 2017-06-09T14:09:53Z | |
date available | 2017-06-09T14:09:53Z | |
date copyright | 1948/06/01 | |
date issued | 1948 | |
identifier issn | 0095-9634 | |
identifier other | ams-13619.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149089 | |
description abstract | On the basis of certain evidence it is concluded that mixing between the cumulus cloud and its environment affects the development of the cloud. It is shown that, for the case of mixing, the lapse rate of temperature within the cloud is greater than the moist-adiabatic rate and also that low relative humidities within the environment disfavor the cloud growth. A synoptic study supports the hypothesis that the forecast of convective showers should take into consideration the relative humidity above the convective condensation level. | |
publisher | American Meteorological Society | |
title | A NOTE ON CUMULUS GROWTH IN A NONSATURATED ENVIRONMENT | |
type | Journal Paper | |
journal volume | 5 | |
journal issue | 3 | |
journal title | Journal of Meteorology | |
identifier doi | 10.1175/1520-0469(1948)005<0103:ANOCGI>2.0.CO;2 | |
journal fristpage | 103 | |
journal lastpage | 107 | |
tree | Journal of Meteorology:;1948:;volume( 005 ):;issue: 003 | |
contenttype | Fulltext |