Show simple item record

dc.contributor.authorMcDonald, James E.
dc.date.accessioned2017-06-09T14:12:19Z
dc.date.available2017-06-09T14:12:19Z
dc.date.copyright1960/04/01
dc.date.issued1960
dc.identifier.issn0095-9634
dc.identifier.otherams-14616.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150197
dc.description.abstractSpectrally averaged infrared absorptivities of thin water films are computed using recent spectrometric results. A water film 5 µ thick irradiated at normal incidence with 0C blackbody radiation is found to have a total absorptivity of 0.49, while, for thicknesses of 10, 50, and 100 µ, the absorptivities are 0.67, 0.92, and 0.95, respectively. Spectrally averaged reflectivity at normal incidence for bulk water is 0.04. Change in the shape of the blackbody emission curve with a change in temperature from 0C to 40C produces negligibly small effect on the spectrally averaged absorptivity and reflectivity. A simple bulk-water method yields infrared cloud absorption half-depths of 17 m for 0.25 g m?3 (and 5 m for 1 g m?3) liquid water content. Only 0.5 per cent is transmitted deeper than 400 m for 0.25 g m?3 or deeper than 100 m for 1 g m?3. Evidence for concluding that Mie-theory effects will tend to reduce these absorption depths to still lower values is presented.
dc.publisherAmerican Meteorological Society
dc.titleABSORPTION OF ATMOSPHERIC RADIATION BY WATER FILMS AND WATER CLOUDS
dc.typeJournal Paper
dc.journal.volume17
dc.journal.issue2
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1960)017<0232:AOARBW>2.0.CO;2
dc.journal.fristpage232
dc.journal.lastpage238
dc.treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 002
dc.contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record