| contributor author | Maccready, P. B. | |
| contributor author | Baughman, R. G. | |
| date accessioned | 2017-06-09T16:54:08Z | |
| date available | 2017-06-09T16:54:08Z | |
| date copyright | 1968/02/01 | |
| date issued | 1968 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-7624.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4218667 | |
| description abstract | Records from an airborne continuous cloud particle collector showed distinct differences in particle characteristics between an unseeded and a seeded cumulus cloud. The unseeded cloud consisted primarily of supercooled water droplets and the seeded cloud entirely of ice particles at the observed levels. Complete glaciation was achieved by AgI seeding even at the relatively warm temperature of ?7C. The AgI acted as efficient ice nuclei even though introduced through a warm cloud base with temperatures above 0C. The observed concentration of crystals was considerably larger than would have been predicted from the standard AgI generator calibration data. Large crystals were observed clustered together in the fully glaciated seeded cloud. | |
| publisher | American Meteorological Society | |
| title | The Glaciation of an AgI-Seeded Cumulus Cloud | |
| type | Journal Paper | |
| journal volume | 7 | |
| journal issue | 1 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1968)007<0132:TGOAAS>2.0.CO;2 | |
| journal fristpage | 132 | |
| journal lastpage | 135 | |
| tree | Journal of Applied Meteorology:;1968:;volume( 007 ):;issue: 001 | |
| contenttype | Fulltext | |