Parameterization of Ice Growth for Numerical Calculations of Cloud DynamicsSource: Monthly Weather Review:;1972:;volume( 100 ):;issue: 006::page 417Author:KOENIG, L. RANDALL
DOI: 10.1175/1520-0493(1972)100<0417:POIGFN>2.3.CO;2Publisher: American Meteorological Society
Abstract: Parametric equations describing the growth of ice particles in the range 10?11?1 g are presented. Three subranges (10?11?5 ? 10?8, 5 ? 10?8?10?4, and 10?4?1 g) are used. The parametric equations were developed with the aid of a complex method of calculating ice-particle growth. Two approaches to using the parametric equations in a simulation resembling a natural cloud situation are described. One method breaks the ice-particle spectrum into three components, the sizes of each being monitored. The other assumes a size distribution that can be characterized by a ?growth-median? size, so that only one size need be monitored to describe the rate of growth. The parametric method is compared with more complicated methods in a simulated cloud environment, and the results are regarded as satisfactory.
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| contributor author | KOENIG, L. RANDALL | |
| date accessioned | 2017-06-09T16:00:01Z | |
| date available | 2017-06-09T16:00:01Z | |
| date copyright | 1972/06/01 | |
| date issued | 1972 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-58449.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4198897 | |
| description abstract | Parametric equations describing the growth of ice particles in the range 10?11?1 g are presented. Three subranges (10?11?5 ? 10?8, 5 ? 10?8?10?4, and 10?4?1 g) are used. The parametric equations were developed with the aid of a complex method of calculating ice-particle growth. Two approaches to using the parametric equations in a simulation resembling a natural cloud situation are described. One method breaks the ice-particle spectrum into three components, the sizes of each being monitored. The other assumes a size distribution that can be characterized by a ?growth-median? size, so that only one size need be monitored to describe the rate of growth. The parametric method is compared with more complicated methods in a simulated cloud environment, and the results are regarded as satisfactory. | |
| publisher | American Meteorological Society | |
| title | Parameterization of Ice Growth for Numerical Calculations of Cloud Dynamics | |
| type | Journal Paper | |
| journal volume | 100 | |
| journal issue | 6 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1972)100<0417:POIGFN>2.3.CO;2 | |
| journal fristpage | 417 | |
| journal lastpage | 423 | |
| tree | Monthly Weather Review:;1972:;volume( 100 ):;issue: 006 | |
| contenttype | Fulltext |