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contributor authorFRITZ, SIGMUND
date accessioned2017-06-09T15:56:09Z
date available2017-06-09T15:56:09Z
date copyright1958/04/01
date issued1958
identifier issn0027-0644
identifier otherams-56994.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197280
description abstractWhen air stagnates in dark polar regions, an inversion forms. The change of the inversion magnitude is studied under the assumption that the snow surface radiates about as much energy as it receives from the atmosphere. It turns out that the inversion magnitude may either decrease or increase as the surface temperature falls, depending on the rate of change of atmospheric ?emissivity? with air temperature.
publisherAmerican Meteorological Society
titleRADIATIONAL INVERSIONS AND SURFACE TEMPERATURE CHANGES
typeJournal Paper
journal volume86
journal issue4
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1958)086<0129:RIASTC>2.0.CO;2
journal fristpage129
journal lastpage131
treeMonthly Weather Review:;1958:;volume( 086 ):;issue: 004
contenttypeFulltext


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