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contributor authorLee, In Young
contributor authorHänel, G.
contributor authorPruppacher, H. R.
date accessioned2017-06-09T14:21:42Z
date available2017-06-09T14:21:42Z
date copyright1980/08/01
date issued1980
identifier issn0022-4928
identifier otherams-17979.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153932
description abstractThe time variation in size of aerosol particles growing by condensation is studied numerically by means of an air parcel model which allows entrainment of air and aerosol particles. Particles of four types of aerosols typically occurring in atmospheric air masses were considered. The present model circumvents any assumption about the size distribution and chemical composition of the aerosol particles by basing the aerosol particle growth on actually observed size distributions and on observed amounts of water taken up under equilibrium by a deposit of the aerosol particles. Characteristic differences in the drop size distribution, liquid water content and supersaturation were found for the clouds which evolved from the four aerosol types considered.
publisherAmerican Meteorological Society
titleA Numerical Determination of the Evolution of Cloud Drop Spectra due to Condensation on Natural Aerosol Particles
typeJournal Paper
journal volume37
journal issue8
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1980)037<1839:ANDOTE>2.0.CO;2
journal fristpage1839
journal lastpage1853
treeJournal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 008
contenttypeFulltext


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