| contributor author | Raymond, D. J. | |
| contributor author | Blyth, A. M. | |
| date accessioned | 2017-06-09T14:31:04Z | |
| date available | 2017-06-09T14:31:04Z | |
| date copyright | 1992/11/01 | |
| date issued | 1992 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-20773.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4157038 | |
| description abstract | The stochastic mixing model of cumulus clouds is extended to the case in which ice and precipitation form. A simple cloud microphysical model is adopted in which ice crystals and aggregates are carried along with the updraft, whereas raindrops, graupel, and hail are assumed to immediately fall out. The model is then applied to the 2 August 1984 case study of convection over the Magdalena Mountains of central New Mexico, with excellent results. The formation of ice and precipitation can explain the transition of this system from a cumulus congestus cloud to a thunderstorm. | |
| publisher | American Meteorological Society | |
| title | Extension of the Stochastic Mixing Model to Cumulonimbus Clouds | |
| type | Journal Paper | |
| journal volume | 49 | |
| journal issue | 21 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1992)049<1968:EOTSMM>2.0.CO;2 | |
| journal fristpage | 1968 | |
| journal lastpage | 1983 | |
| tree | Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 021 | |
| contenttype | Fulltext | |