| contributor author | Williams, E. R. | |
| contributor author | Zhang, R. | |
| contributor author | Rydock, J. | |
| date accessioned | 2017-06-09T14:30:33Z | |
| date available | 2017-06-09T14:30:33Z | |
| date copyright | 1991/10/01 | |
| date issued | 1991 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-20606.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4156853 | |
| description abstract | A number of experimental studies have shown that sublimating ice acquires negative charge and ice undergoing vapor deposition acquires positive charge. Microphysical calculations are performed to determine the diffusional state (i.e., sublimation versus deposition) of riming graupel particles. Comparisons with earlier laboratory measurements of charge transfer to a rotating rimer in a cloud of supercooled water droplets and ice crystals again suggest that sublimating graupel particles charge negatively and graupel undergoing deposition charge positively. Implications for charge separation in thunderstorms are discussed. | |
| publisher | American Meteorological Society | |
| title | Mixed-Phase Microphysics and Cloud Electrification | |
| type | Journal Paper | |
| journal volume | 48 | |
| journal issue | 19 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1991)048<2195:MPMACE>2.0.CO;2 | |
| journal fristpage | 2195 | |
| journal lastpage | 2203 | |
| tree | Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 019 | |
| contenttype | Fulltext | |