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dc.contributor.authorMather, Graeme K.
dc.contributor.authorMorrison, Brian J.
dc.contributor.authorMorgan, Griffith M.
dc.date.accessioned2017-06-09T14:01:29Z
dc.date.available2017-06-09T14:01:29Z
dc.date.copyright1986/11/01
dc.date.issued1986
dc.identifier.issn0733-3021
dc.identifier.otherams-11092.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146282
dc.description.abstractFor 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.publisherAmerican Meteorological Society
dc.titleA Preliminary Assessment of the Importance of Coalescence in Convective Clouds of the Eastern Transvaal
dc.typeJournal Paper
dc.journal.volume25
dc.journal.issue11
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1986)025<1780:APAOTI>2.0.CO;2
dc.journal.fristpage1780
dc.journal.lastpage1784
dc.treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 011
dc.contenttypeFulltext


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