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contributor authorMossop, S. C.
contributor authorRuskin, R. E.
contributor authorHeffernan, K. J.
date accessioned2017-06-09T14:14:37Z
date available2017-06-09T14:14:37Z
date copyright1968/09/01
date issued1968
identifier issn0022-4928
identifier otherams-15502.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151182
description abstractA long-lived cumulus cloud off the southern coast of Australia was found to contain ice crystals, even though the coldest temperature in it was about ?4C. Two instrumented aircraft made successive passes through the cloud and continuous samplers were used to replicate cloud particles. It was found that columnar crystals were present in concentrations up to 100 liter?1. This was at least three orders of magnitude greater than the expected concentration of active ice nuclei as determined by cloud chamber measurements made under the base of the same cloud. It appears that some ice crystal multiplication mechanism was at work, though the exact nature of the process cannot be decided on available evidence.
publisherAmerican Meteorological Society
titleGlaciation of a Cumulus at Approximately −4C
typeJournal Paper
journal volume25
journal issue5
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1968)025<0889:GOACAA>2.0.CO;2
journal fristpage889
journal lastpage899
treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 005
contenttypeFulltext


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