| dc.contributor.author | Mather, Graeme K. | |
| dc.contributor.author | Morrison, Brian J. | |
| dc.contributor.author | Morgan, Griffith M. | |
| dc.date.accessioned | 2017-06-09T14:01:29Z | |
| dc.date.available | 2017-06-09T14:01:29Z | |
| dc.date.copyright | 1986/11/01 | |
| dc.date.issued | 1986 | |
| dc.identifier.issn | 0733-3021 | |
| dc.identifier.other | ams-11092.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4146282 | |
| dc.description.abstract | For the past three years, a Learjet has been making microphysical measurements in new cloud development on the flanks of multicellular storms in the eastern Transvaal area of South Africa. Data from an imaging probe and a forward scattering spectrometer have been averaged for each storm for all first cloud penetrations between ?8° and ?12°C. Clear images of drops of diameters greater than 300 ?m are found in 40% of the 42 storms measured. Most of the observed drops are associated with the more ?maritime? droplet spectra. Also, the appearance of coalescence around ?10°C appears to be related to cloud base temperatures and buoyancies, rather than changes in air masses, suggesting that cloud thermodynamics may play a dominant role in determining cloud microphysics in the Nelspruit area. | |
| dc.publisher | American Meteorological Society | |
| dc.title | A Preliminary Assessment of the Importance of Coalescence in Convective Clouds of the Eastern Transvaal | |
| dc.type | Journal Paper | |
| dc.journal.volume | 25 | |
| dc.journal.issue | 11 | |
| dc.journal.title | Journal of Climate and Applied Meteorology | |
| dc.identifier.doi | 10.1175/1520-0450(1986)025<1780:APAOTI>2.0.CO;2 | |
| dc.journal.fristpage | 1780 | |
| dc.journal.lastpage | 1784 | |
| dc.tree | Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 011 | |
| dc.contenttype | Fulltext | |