| contributor author | Johnson, David B. | |
| date accessioned | 2017-06-09T14:22:52Z | |
| date available | 2017-06-09T14:22:52Z | |
| date copyright | 1982/02/01 | |
| date issued | 1982 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-18300.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4154291 | |
| description abstract | Giant and ultragiant aerosol particles can play an important role in warm rain initiation. Recent aerosol measurements have established that particles as large as 100 ?m are a regular part of the atmospheric aerosol. When ingested in growing clouds, these particles will produce a tail of large drops on the upper end of the cloud-droplet distribution. In a series of numerical computations, this tail of large drops was found to be a significant destabilizing factor which can speed precipitation development. | |
| publisher | American Meteorological Society | |
| title | The Role of Giant and Ultragiant Aerosol Particles in Warm Rain Initiation | |
| type | Journal Paper | |
| journal volume | 39 | |
| journal issue | 2 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1982)039<0448:TROGAU>2.0.CO;2 | |
| journal fristpage | 448 | |
| journal lastpage | 460 | |
| tree | Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 002 | |
| contenttype | Fulltext | |
