| contributor author | Mossop, S. C. | |
| date accessioned | 2017-06-09T14:40:14Z | |
| date available | 2017-06-09T14:40:14Z | |
| date copyright | 1985/03/01 | |
| date issued | 1985 | |
| identifier issn | 0003-0007 | |
| identifier other | ams-24111.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4160748 | |
| description abstract | Ice crystals in supercooled clouds may form upon ice nuclei, or they may arise through secondary processes. Two of these secondary ice ?multiplication? mechanisms are discussed in some detail: the rime-splintering process and the mechanical fracture of ice particles. The nature of the water-drop size distribution has an important bearing on secondary ice production. Confident predictions of ice particle concentration can only be made in a few limited cloud situations. This is a serious handicap in assessing the feasibility of artificial rainmaking through the ice crystal process. | |
| publisher | American Meteorological Society | |
| title | The Origin and Concentration of Ice Crystals in Clouds | |
| type | Journal Paper | |
| journal volume | 66 | |
| journal issue | 3 | |
| journal title | Bulletin of the American Meteorological Society | |
| identifier doi | 10.1175/1520-0477(1985)066<0264:TOACOI>2.0.CO;2 | |
| journal fristpage | 264 | |
| journal lastpage | 273 | |
| tree | Bulletin of the American Meteorological Society:;1985:;volume( 066 ):;issue: 003 | |
| contenttype | Fulltext | |
