| contributor author | Wang, P. K. | |
| contributor author | Pruppacher, H. R. | |
| date accessioned | 2017-06-09T17:38:59Z | |
| date available | 2017-06-09T17:38:59Z | |
| date copyright | 1977/03/01 | |
| date issued | 1977 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-9240.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4232707 | |
| description abstract | A theoretical method is given which allows computing the acceleration to terminal velocity of cloud and raindrops at various levels in the atmosphere. For drops of equivalent radius 800 ?m ≤ a0 ≤ 3500 ?m our theoretical predictions were found to agree well with the results of an experimental study carried out in the UCLA Rain-Shaft. For drops of 20 ?m ≤ a0 ≤ 80 ?m our theoretical predictions were found to agree well with the experimental results of Sartor and Abbott (1975). Experiment and theory indicate that in air of 1000 mb and 20°C, drops of a0 > 1000 ?m need distances of at least 12 m to accelerate to terminal velocity. | |
| publisher | American Meteorological Society | |
| title | Acceleration to Terminal Velocity of Cloud and Raindrops | |
| type | Journal Paper | |
| journal volume | 16 | |
| journal issue | 3 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1977)016<0275:ATTVOC>2.0.CO;2 | |
| journal fristpage | 275 | |
| journal lastpage | 280 | |
| tree | Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 003 | |
| contenttype | Fulltext | |
