## Abstract Computations are made of the radar reflectivity __Z__~__e__~ of particles present in hailstorm updraughts in exponential size spectra. The reflectivity varies substantially according to the radar wavelength and according to whether the particles are wet or dry. In severe storms a very s
Radar reflectivity of lightning-induced plasmas
β Scribed by M.C. Lee; Y.R. Dalkir; E.R. Williams
- Publisher
- Elsevier Science
- Year
- 1998
- Tongue
- English
- Weight
- 314 KB
- Volume
- 60
- Category
- Article
- ISSN
- 1364-6826
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β¦ Synopsis
The scattering of radio waves from lightning!induced plasmas is investigated[ The plasmas are modeled as long\ perfectly conducting cylinders with surface density irregularities on a scale much smaller than the total channel length[ The theoretical wavelength dependence of the radar re~ectivity is compared with experimental results obtained with the MIT C!band and S!band radars[ It is found that the theory of rough surface scattering predicts two types of inverse power law wavelength dependence for radar re~ectivity[ They are 0:l and 0:l 1 \ which correspond to density ~uctuations of lightning plasmas with a Gaussian type spectrum and a power!law type spectrum\ respectively[ By contrast\ the theory of long\ thin conductors predicts a wavelength dependence of l 9[4 for radar re~ectivity[ The experimental observations on common lightning targets free of precipitation masking e}ects show a mean wavelength dependence of 0:l 9[73 [ The observed wavelength dependence lies between the predictions of the two theories[ It indicates that the wavelength dependence in these observations is bounded by these two theories[ We conclude that the proposed theory for fat overdense plasma channels with irregular surfaces and the theory for long\ thin overdense channels bracket the observed wavelength dependence[ Γ 0887 Elsevier Science Ltd[ All rights reserved[
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## Abstract Weather radar signals fluctuate because of relative motions among the scatterers; these fluctuations must be accounted for in quantitative reflectivity measurements. The standard theory of weather signal fluctuations assumes targets of fixed reflectivity. In actual measurements, signals