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contributor authorAckerman, Steven A.
contributor authorStephens, Graeme L.
date accessioned2017-06-09T14:27:23Z
date available2017-06-09T14:27:23Z
date copyright1987/06/01
date issued1987
identifier issn0022-4928
identifier otherams-19552.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155681
description abstractIn this paper we demonstrate that the anomalous diffraction theory of van de Hulst with some modifications, provides a reasonable approximation of the volume extinction and absorption coefficients. We also show how the shortwave radiative properties of a water cloud can be derived in terms of 1) cloud liquid water path, 2) the effective radius of the droplet distribution, and 3) the balk absorption coefficient of water. With the aid of the approximate diffraction theory we describe how cloud albedo and shortwave absorption depend on the droplet size. We demonstrate this dependence to be somewhat complex and show that the variation of absorption with variation of droplet size depends also on the cloud liquid water path. For ?deep? or semi-infinite clouds, absorption increases monotonically with increasing effective radius, but the reverse dependence is established for thin clouds. The implications of these results to the so-called absorption paradox and to the possibility of determining droplet size information from remotely measured reflectance spectra are also discussed.
publisherAmerican Meteorological Society
titleThe Absorption of Solar Radiation by Cloud Droplets: An Application of Anomalous Diffraction Theory
typeJournal Paper
journal volume44
journal issue12
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1987)044<1574:TAOSRB>2.0.CO;2
journal fristpage1574
journal lastpage1588
treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 012
contenttypeFulltext


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