Analytic Studies of Cloud Droplet Coalescence ISource: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 001::page 54Author:Scott, William T.
DOI: 10.1175/1520-0469(1968)025<0054:ASOCDC>2.0.CO;2Publisher: American Meteorological Society
Abstract: The kinetic equation for the pure growth-by-coalescence process is solved exactly for three types of overall collection probability: proportional to the sum of droplet volumes, proportional to the product of droplet volumes, and constant. Series and asymptotic expressions are given for a variety of initial conditions, and methods indicated for use of arbitrary initial functions. Calculations are presented for initial volume distributions equivalent to Gaussian distributions in radius with σ/? = 0.37, O.25, 0.15 and O.123, and several stages of real time from 69 to 1600 sec. We assume 1 gm m?8 water content, a mean volume radius of 10 ?, and normalization of the collection efficiency formulas to fit those of Shafrir and Neiburger for a 30?10 ? collision.
|
Collections
Show full item record
| contributor author | Scott, William T. | |
| date accessioned | 2017-06-09T14:14:17Z | |
| date available | 2017-06-09T14:14:17Z | |
| date copyright | 1968/01/01 | |
| date issued | 1968 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-15386.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4151052 | |
| description abstract | The kinetic equation for the pure growth-by-coalescence process is solved exactly for three types of overall collection probability: proportional to the sum of droplet volumes, proportional to the product of droplet volumes, and constant. Series and asymptotic expressions are given for a variety of initial conditions, and methods indicated for use of arbitrary initial functions. Calculations are presented for initial volume distributions equivalent to Gaussian distributions in radius with σ/? = 0.37, O.25, 0.15 and O.123, and several stages of real time from 69 to 1600 sec. We assume 1 gm m?8 water content, a mean volume radius of 10 ?, and normalization of the collection efficiency formulas to fit those of Shafrir and Neiburger for a 30?10 ? collision. | |
| publisher | American Meteorological Society | |
| title | Analytic Studies of Cloud Droplet Coalescence I | |
| type | Journal Paper | |
| journal volume | 25 | |
| journal issue | 1 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1968)025<0054:ASOCDC>2.0.CO;2 | |
| journal fristpage | 54 | |
| journal lastpage | 65 | |
| tree | Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 001 | |
| contenttype | Fulltext |