RADIATIONAL INVERSIONS AND SURFACE TEMPERATURE CHANGESSource: Monthly Weather Review:;1958:;volume( 086 ):;issue: 004::page 129Author:FRITZ, SIGMUND
DOI: 10.1175/1520-0493(1958)086<0129:RIASTC>2.0.CO;2Publisher: American Meteorological Society
Abstract: When 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.
|
Collections
Show full item record
| contributor author | FRITZ, SIGMUND | |
| date accessioned | 2017-06-09T15:56:09Z | |
| date available | 2017-06-09T15:56:09Z | |
| date copyright | 1958/04/01 | |
| date issued | 1958 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-56994.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4197280 | |
| description abstract | When 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. | |
| publisher | American Meteorological Society | |
| title | RADIATIONAL INVERSIONS AND SURFACE TEMPERATURE CHANGES | |
| type | Journal Paper | |
| journal volume | 86 | |
| journal issue | 4 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1958)086<0129:RIASTC>2.0.CO;2 | |
| journal fristpage | 129 | |
| journal lastpage | 131 | |
| tree | Monthly Weather Review:;1958:;volume( 086 ):;issue: 004 | |
| contenttype | Fulltext |