TIROS II Window Radiation and Large Scale Vertical MotionSource: Journal of Applied Meteorology:;1963:;volume( 002 ):;issue: 006::page 770Author:Shenk, William E.
DOI: 10.1175/1520-0450(1963)002<0770:TIWRAL>2.0.CO;2Publisher: American Meteorological Society
Abstract: The difference between observed window radiation and radiation expected without clouds was related to various synoptic parameter. The but correlation, 0.72, was obtained with vertical motion computed by the adiabatic methods at 700 mb. Other variables tested were meridional flow and vertical motion at other level.
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| contributor author | Shenk, William E. | |
| date accessioned | 2017-06-09T16:34:29Z | |
| date available | 2017-06-09T16:34:29Z | |
| date copyright | 1963/12/01 | |
| date issued | 1963 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-7025.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4212012 | |
| description abstract | The difference between observed window radiation and radiation expected without clouds was related to various synoptic parameter. The but correlation, 0.72, was obtained with vertical motion computed by the adiabatic methods at 700 mb. Other variables tested were meridional flow and vertical motion at other level. | |
| publisher | American Meteorological Society | |
| title | TIROS II Window Radiation and Large Scale Vertical Motion | |
| type | Journal Paper | |
| journal volume | 2 | |
| journal issue | 6 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1963)002<0770:TIWRAL>2.0.CO;2 | |
| journal fristpage | 770 | |
| journal lastpage | 775 | |
| tree | Journal of Applied Meteorology:;1963:;volume( 002 ):;issue: 006 | |
| contenttype | Fulltext |