ICE-CRYSTAL GROWTHSource: Journal of Meteorology:;1952:;volume( 009 ):;issue: 001::page 36Author:Reynolds, S. E.
DOI: 10.1175/1520-0469(1952)009<0036:ICG>2.0.CO;2Publisher: American Meteorological Society
Abstract: Laboratory measurements of the rate of ice-crystal growth by sublimation are found to be in good agreement with Houghton's (1950) calculations. With use of Houghton's data for the growth of ice crystals at relatively warm temperatures, and Vonnegut's (1949) data for the reaction rate of silver-iodide particles as sublimation nuclei, it is shown that it is extremely unlikely that summer convective clouds can be overseeded with ground generators.
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| contributor author | Reynolds, S. E. | |
| date accessioned | 2017-06-09T14:10:31Z | |
| date available | 2017-06-09T14:10:31Z | |
| date copyright | 1952/02/01 | |
| date issued | 1952 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-13884.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149383 | |
| description abstract | Laboratory measurements of the rate of ice-crystal growth by sublimation are found to be in good agreement with Houghton's (1950) calculations. With use of Houghton's data for the growth of ice crystals at relatively warm temperatures, and Vonnegut's (1949) data for the reaction rate of silver-iodide particles as sublimation nuclei, it is shown that it is extremely unlikely that summer convective clouds can be overseeded with ground generators. | |
| publisher | American Meteorological Society | |
| title | ICE-CRYSTAL GROWTH | |
| type | Journal Paper | |
| journal volume | 9 | |
| journal issue | 1 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1952)009<0036:ICG>2.0.CO;2 | |
| journal fristpage | 36 | |
| journal lastpage | 40 | |
| tree | Journal of Meteorology:;1952:;volume( 009 ):;issue: 001 | |
| contenttype | Fulltext |