| contributor author | Du, Shumung | |
| contributor author | Wilson, John D. | |
| date accessioned | 2017-06-09T14:33:30Z | |
| date available | 2017-06-09T14:33:30Z | |
| date copyright | 1995/11/01 | |
| date issued | 1995 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-21617.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4157976 | |
| description abstract | From an analysis of scales in the cloud droplet collision problem, the authors infer that a trajectory model that is to be capable of predicting collisions between droplets of all possible sizes should be of second-order, that is should explicitly model particle acceleration. But for collisions between large droplets (radius about 50 µm or larger), which are still much smaller than raindroplets, a first-order model is appropriate. The relative motion of large droplets are studied with a first-order, two particle trajectory model. Turbulence is found to be unimportant (relative to differential gravitational settling) if the (large) droplet sizes are sufficiently distinct. Zeroth-order two-particle models, of the type hitherto applied to be problem, deteriorate in accuracy as the influence of turbulence on the droplet separation increases, that is, for large σv/v?, where σv is the turbulent velocity scale and v? is the droplet still-air terminal velocity. Under no circumstance is a single-particle model applicable. | |
| publisher | American Meteorological Society | |
| title | Modelling the Effect of Turbulence on the Collision of Cloud Droplets | |
| type | Journal Paper | |
| journal volume | 52 | |
| journal issue | 22 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1995)052<3849:MTEOTO>2.0.CO;2 | |
| journal fristpage | 3849 | |
| journal lastpage | 3856 | |
| tree | Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 022 | |
| contenttype | Fulltext | |