Numerical Modeling of Ice DepositionSource: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 002::page 226Author:Koenig, L. R.
DOI: 10.1175/1520-0469(1971)028<0226:NMOID>2.0.CO;2Publisher: American Meteorological Society
Abstract: A method of computing the rate of growth of ice crystals by deposition is described. Predictions of growth characteristics over the temperature range of ?1 through ?35C are shown and compared with meager experimental data available within this temperature range. The growth rate equations are based on Fick's law of diffusion. In applying this law to nonspherical ice crystals, the analogy between an electrostatic potential field surrounding a charged body and the vapor-density field surrounding a similarly shaped ice crystal is utilized. Allowances are made for effects of forced convection caused by the movement of the crystal through the air and the change in shape and bulk density of the ice crystal; these effects are predicted to be of significant importance. A simple, empirical equation using two temperature-dependent parameters was found to describe the crystal growth rate as a, function of mass. For many cases where only the rate of mass conversion from vapor to solid is required, the simple equation is believed satisfactory.
|
Collections
Show full item record
| contributor author | Koenig, L. R. | |
| date accessioned | 2017-06-09T14:15:45Z | |
| date available | 2017-06-09T14:15:45Z | |
| date copyright | 1971/03/01 | |
| date issued | 1971 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-15923.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4151649 | |
| description abstract | A method of computing the rate of growth of ice crystals by deposition is described. Predictions of growth characteristics over the temperature range of ?1 through ?35C are shown and compared with meager experimental data available within this temperature range. The growth rate equations are based on Fick's law of diffusion. In applying this law to nonspherical ice crystals, the analogy between an electrostatic potential field surrounding a charged body and the vapor-density field surrounding a similarly shaped ice crystal is utilized. Allowances are made for effects of forced convection caused by the movement of the crystal through the air and the change in shape and bulk density of the ice crystal; these effects are predicted to be of significant importance. A simple, empirical equation using two temperature-dependent parameters was found to describe the crystal growth rate as a, function of mass. For many cases where only the rate of mass conversion from vapor to solid is required, the simple equation is believed satisfactory. | |
| publisher | American Meteorological Society | |
| title | Numerical Modeling of Ice Deposition | |
| type | Journal Paper | |
| journal volume | 28 | |
| journal issue | 2 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1971)028<0226:NMOID>2.0.CO;2 | |
| journal fristpage | 226 | |
| journal lastpage | 237 | |
| tree | Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 002 | |
| contenttype | Fulltext |