Note on Nocturnal Radiation ReversalSource: Monthly Weather Review:;1972:;volume( 100 ):;issue: 005::page 354Author:CLARKE, REGINALD H.
DOI: 10.1175/1520-0493(1972)100<0354:NONRR>2.3.CO;2Publisher: American Meteorological Society
Abstract: Nocturnal 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.
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contributor author | CLARKE, REGINALD H. | |
date accessioned | 2017-06-09T15:59:59Z | |
date available | 2017-06-09T15:59:59Z | |
date copyright | 1972/05/01 | |
date issued | 1972 | |
identifier issn | 0027-0644 | |
identifier other | ams-58440.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4198887 | |
description abstract | Nocturnal 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. | |
publisher | American Meteorological Society | |
title | Note on Nocturnal Radiation Reversal | |
type | Journal Paper | |
journal volume | 100 | |
journal issue | 5 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/1520-0493(1972)100<0354:NONRR>2.3.CO;2 | |
journal fristpage | 354 | |
journal lastpage | 356 | |
tree | Monthly Weather Review:;1972:;volume( 100 ):;issue: 005 | |
contenttype | Fulltext |