| contributor author | Douglass, Anne R. | |
| contributor author | Stanford, John L. | |
| date accessioned | 2017-06-09T17:40:19Z | |
| date available | 2017-06-09T17:40:19Z | |
| date copyright | 1980/01/01 | |
| date issued | 1979 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-9838.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4233370 | |
| description abstract | It is shown that the gradient of satellite-derived radiance is proportional to a certain vertical integral of the geostrophic wind. The radiance gradient is shown to be useful in locating the upper tropospheric jet maxima in middle latitudes; the major uncertainty results from lack of specific knowledge of the lower stratospheric winds above the area in question. At high latitudes, the radiance gradient delineates regions of stratospheric jet maxima. | |
| publisher | American Meteorological Society | |
| title | The Relationship between the Gradient of Satellite-Derived Radiance and Upper Tropospheric/Lower Stratospheric Winds | |
| type | Journal Paper | |
| journal volume | 19 | |
| journal issue | 1 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1980)019<0113:TRBTGO>2.0.CO;2 | |
| journal fristpage | 113 | |
| journal lastpage | 115 | |
| tree | Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 001 | |
| contenttype | Fulltext | |