| contributor author | Rosinski, J. | |
| contributor author | Nagamoto, C. T. | |
| contributor author | Kerrigan, T. C. | |
| contributor author | Langer, G. | |
| date accessioned | 2017-06-09T14:16:56Z | |
| date available | 2017-06-09T14:16:56Z | |
| date copyright | 1973/05/01 | |
| date issued | 1973 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-16371.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4152147 | |
| description abstract | The majority of hydrosol particles in the submicron range in precipitation are produced by separation from the surfaces of larger hydrosolized aerosol particles. Sail particles may produce freezing nuclei active between ?10 and ?7C in concentrations up to 100 cm?3 per soil particle, and freezing nuclei active at temperatures warmer than ?20C in concentrations greater than 1000 cm?3 per soil particle. It is concluded that neither the role of freezing nuclei in the development of precipitation nor even the distribution of freezing nuclei among cloud particles, raindrops and hailstones can be deduced from the determination of freezing nucleus populations in bulk precipitation samples. | |
| publisher | American Meteorological Society | |
| title | Freezing Nuclei Derived from Soil Particles | |
| type | Journal Paper | |
| journal volume | 30 | |
| journal issue | 4 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1973)030<0644:FNDFSP>2.0.CO;2 | |
| journal fristpage | 644 | |
| journal lastpage | 652 | |
| tree | Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 004 | |
| contenttype | Fulltext | |
