| contributor author | Hsieh, Yi-Ping | |
| date accessioned | 2017-06-09T14:10:18Z | |
| date available | 2017-06-09T14:10:18Z | |
| date copyright | 1950/12/01 | |
| date issued | 1950 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-13797.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149286 | |
| description abstract | The vertical circulation and the changes of atmospheric structure during the formation of a shear line in the upper atmosphere are studied. The vertical distribution of divergence and convergence at the trough line is determined, assuming adiabatic processes. A scheme for the process of formation of an upper shear-line is proposed. A comparison of this process with that involved in the formation of upper cut-off cold lows is presented. | |
| publisher | American Meteorological Society | |
| title | ON THE FORMATION OF SHEAR LINES IN THE UPPER ATMOSPHERE | |
| type | Journal Paper | |
| journal volume | 7 | |
| journal issue | 6 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1950)007<0382:OTFOSL>2.0.CO;2 | |
| journal fristpage | 382 | |
| journal lastpage | 387 | |
| tree | Journal of Meteorology:;1950:;volume( 007 ):;issue: 006 | |
| contenttype | Fulltext | |
