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contributor authorHeymsfield, Gerald M.
date accessioned2017-06-09T17:38:44Z
date available2017-06-09T17:38:44Z
date copyright1976/09/01
date issued1976
identifier issn0021-8952
identifier otherams-9143.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232599
description abstractVertical incidence Doppler radar observations of an evaporating ice crystal cloud revealed many multimodal Doppler spectra, with modes often separated by more than 1 m s?1, and unusually large variances. The observations are explained in terms of a vertical velocity field consisting of a plane wave motion on sub-beam scales, and a larger scale horizontal shear of the vertical wind. Doppler spectra and variances of the proposed model of the vertical velocity are presented.
publisherAmerican Meteorological Society
titleExplanation of Multimodal Doppler Spectra in Terms of Sub-Beam Scale Motions
typeJournal Paper
journal volume15
journal issue9
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1976)015<0976:EOMDSI>2.0.CO;2
journal fristpage976
journal lastpage981
treeJournal of Applied Meteorology:;1976:;volume( 015 ):;issue: 009
contenttypeFulltext


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