Show simple item record

contributor authorGiddings, W. P.
contributor authorBaker, M. B.
date accessioned2017-06-09T14:19:53Z
date available2017-06-09T14:19:53Z
date copyright1977/12/01
date issued1977
identifier issn0022-4928
identifier otherams-17400.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153291
description abstractHaze particles coated by organic substances have been found in some maritime regions. It is shown that the most likely origin of surfactant material on atmospheric droplets is the ocean surface, which contains fatty acids and other organics previously identified in atmospheric aerosol particles as well as calcium soaps and proteinaceous substances which could act as surfactants. Persistent hazes, but not fogs, may result from stabilization of unactivated atmospheric droplets by organic surfactants in maritime regions. Calculations show that under time-varying atmospheric conditions the primary effect of surfactants is to decrease the steady-state portion of. the growth rate. A kinetic mechanism is proposed for the monolayer inhibitory action, implying limitations on the utility of the accommodation coefficient formulation.
publisherAmerican Meteorological Society
titleSources and Effects of Monolayers on Atmospheric Water Droplets
typeJournal Paper
journal volume34
journal issue12
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1977)034<1957:SAEOMO>2.0.CO;2
journal fristpage1957
journal lastpage1964
treeJournal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 012
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record