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contributor authorCLARKE, REGINALD H.
date accessioned2017-06-09T15:59:59Z
date available2017-06-09T15:59:59Z
date copyright1972/05/01
date issued1972
identifier issn0027-0644
identifier otherams-58440.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198887
description abstractNocturnal radiation reversal is essentially an unsteady, advective effect. It requires that clouds or fog drift over a previously cooled surface. In the case of higher clouds, reversal can occur only with a sufficiently intense surface temperature inversion. Statistics of authentic cases of reversal occurring at Aspendale, Australia (38°02?S, 138°06?E), are given and related to other meteorological variables.
publisherAmerican Meteorological Society
titleNote on Nocturnal Radiation Reversal
typeJournal Paper
journal volume100
journal issue5
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1972)100<0354:NONRR>2.3.CO;2
journal fristpage354
journal lastpage356
treeMonthly Weather Review:;1972:;volume( 100 ):;issue: 005
contenttypeFulltext


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