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dc.contributor.authorWeger, Eric
dc.date.accessioned2017-06-09T14:12:18Z
dc.date.available2017-06-09T14:12:18Z
dc.date.copyright1960/04/01
dc.date.issued1960
dc.identifier.issn0095-9634
dc.identifier.otherams-14609.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150189
dc.description.abstractThe problem of atmospheric radiation over narrow bands in the microwave region is considered. Equations for the radiation received at a point on the earth's surface for a particular angle of observation, and also for the integrated average over the whole sky, are presented. For convenience, the results are expressed as ?apparent sky temperatures??the comparison being a black body. The dependence of the sky temperatures on wavelength and weather conditions is brought out by a discussion of the absorption of radiation by oxygen, water vapor and condensed water droplets. Calculated sky temperature data are presented for three typical weather conditions at wavelengths of 0.30, 0.43, 0.86, 1.25, 1.80 and 3.00 cm. The causes of the wide range of temperatures encountered at these wavelengths for various sky conditions are discussed.
dc.publisherAmerican Meteorological Society
dc.titleAPPARENT SKY TEMPERATURES IN THE MICROWAVE REGION
dc.typeJournal Paper
dc.journal.volume17
dc.journal.issue2
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1960)017<0159:ASTITM>2.0.CO;2
dc.journal.fristpage159
dc.journal.lastpage165
dc.treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 002
dc.contenttypeFulltext


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