contributor author | Giddings, W. P. | |
contributor author | Baker, M. B. | |
date accessioned | 2017-06-09T14:19:53Z | |
date available | 2017-06-09T14:19:53Z | |
date copyright | 1977/12/01 | |
date issued | 1977 | |
identifier issn | 0022-4928 | |
identifier other | ams-17400.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4153291 | |
description abstract | Haze 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. | |
publisher | American Meteorological Society | |
title | Sources and Effects of Monolayers on Atmospheric Water Droplets | |
type | Journal Paper | |
journal volume | 34 | |
journal issue | 12 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1977)034<1957:SAEOMO>2.0.CO;2 | |
journal fristpage | 1957 | |
journal lastpage | 1964 | |
tree | Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 012 | |
contenttype | Fulltext | |