On the Motion of a Three-Dimensional Quasi-Steady Convective Storm in ShearSource: Monthly Weather Review:;1978:;volume( 106 ):;issue: 011::page 1622Author:Haman, K. E.
DOI: 10.1175/1520-0493(1978)106<1622:OTMOAT>2.0.CO;2Publisher: American Meteorological Society
Abstract: From the hypothesis that a quasi-steady convective storm adjusts its internal flow to the ambient wind field, the velocity of the storm motion can be calculated by means of the Bernoulli equation. This velocity may be fairly dependent on the process of formation and discharge of precipitation.
|
Collections
Show full item record
| contributor author | Haman, K. E. | |
| date accessioned | 2017-06-09T16:02:16Z | |
| date available | 2017-06-09T16:02:16Z | |
| date copyright | 1978/11/01 | |
| date issued | 1978 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-59397.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4199950 | |
| description abstract | From the hypothesis that a quasi-steady convective storm adjusts its internal flow to the ambient wind field, the velocity of the storm motion can be calculated by means of the Bernoulli equation. This velocity may be fairly dependent on the process of formation and discharge of precipitation. | |
| publisher | American Meteorological Society | |
| title | On the Motion of a Three-Dimensional Quasi-Steady Convective Storm in Shear | |
| type | Journal Paper | |
| journal volume | 106 | |
| journal issue | 11 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1978)106<1622:OTMOAT>2.0.CO;2 | |
| journal fristpage | 1622 | |
| journal lastpage | 1627 | |
| tree | Monthly Weather Review:;1978:;volume( 106 ):;issue: 011 | |
| contenttype | Fulltext |