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contributor authorBattan, Louis J.
contributor authorTheiss, John B.
date accessioned2017-06-09T17:27:44Z
date available2017-06-09T17:27:44Z
date copyright1973/06/01
date issued1973
identifier issn0021-8952
identifier otherams-8568.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229155
description abstractAn X-band pulsed-Doppler radar having its beam fixed at an elevation angle of 3°, has supplied new data on radial velocity spectra in two showers. It was found that the mean Doppler velocity, variance of the Doppler spectrum, and radar reflectivity varied markedly over distances of less than a kilometer. The observed variances were less than about 1 m2 sec?2 in more than 80% of the observations and exceeded 3 m2 sec?2 in about 4% of the cases. An analysis of ?V?/?r, the radial gradient of the mean Doppler velocity, yielded a nearly Gaussian curve having a mean of 0.2 ? 10?2 sec?1 and a standard deviation of 5.8 ? 10?3 sec?1. The effects of the radial gradient of the radial wind apparently can explain less than about 15% of the observed variance of the Doppler spectrum. It appears that a major part of the variance is attributable to scales of motion smaller than the dimensions of the sampling volume.
publisherAmerican Meteorological Society
titleWind Gradients and Variance of Doppler Spectra in Showers Viewed Horizontally
typeJournal Paper
journal volume12
journal issue4
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1973)012<0688:WGAVOD>2.0.CO;2
journal fristpage688
journal lastpage693
treeJournal of Applied Meteorology:;1973:;volume( 012 ):;issue: 004
contenttypeFulltext


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