ENTRAINMENT OF AIR INTO A CUMULUS CLOUDSource: Journal of Meteorology:;1947:;volume( 004 ):;issue: 003::page 91Author:Stommel, Henry
DOI: 10.1175/1520-0469(1947)004<0091:EOAIAC>2.0.CO;2Publisher: American Meteorological Society
Abstract: A theory of convective clouds is presented, the fundamental hypothesis being that the ascending current in a cloud entrains air from its surroundings. A method is developed for computing the amount of entrainment from a knowledge of the temperature and specific humidity inside and outside the cloud. The concentration of water in the form of drops is also determined. Finally the theory is applied to some observations of trade cumulus made near San Juan, Puerto Rico.
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contributor author | Stommel, Henry | |
date accessioned | 2017-06-09T14:09:47Z | |
date available | 2017-06-09T14:09:47Z | |
date copyright | 1947/06/01 | |
date issued | 1947 | |
identifier issn | 0095-9634 | |
identifier other | ams-13581.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149047 | |
description abstract | A theory of convective clouds is presented, the fundamental hypothesis being that the ascending current in a cloud entrains air from its surroundings. A method is developed for computing the amount of entrainment from a knowledge of the temperature and specific humidity inside and outside the cloud. The concentration of water in the form of drops is also determined. Finally the theory is applied to some observations of trade cumulus made near San Juan, Puerto Rico. | |
publisher | American Meteorological Society | |
title | ENTRAINMENT OF AIR INTO A CUMULUS CLOUD | |
type | Journal Paper | |
journal volume | 4 | |
journal issue | 3 | |
journal title | Journal of Meteorology | |
identifier doi | 10.1175/1520-0469(1947)004<0091:EOAIAC>2.0.CO;2 | |
journal fristpage | 91 | |
journal lastpage | 94 | |
tree | Journal of Meteorology:;1947:;volume( 004 ):;issue: 003 | |
contenttype | Fulltext |