Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengths

Polarimetric radar variables of rainfall events, like differential reflectivity <i>Z</i><sub>DR</sub>, or specific differential phase <i>K</i><sub>DP</sub>, are better suited for estimatin...

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Main Authors: F. Teschl, W. L. Randeu, M. Schönhuber, R. Teschl
Format: Article
Language:English
Published: Copernicus Publications 2008-04-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/16/27/2008/adgeo-16-27-2008.pdf
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spelling doaj-dee7bde5fc41450384c2b55bda686dcf2020-11-25T00:57:53ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592008-04-01162732Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengthsF. TeschlW. L. RandeuM. SchönhuberR. TeschlPolarimetric radar variables of rainfall events, like differential reflectivity <i>Z</i><sub>DR</sub>, or specific differential phase <i>K</i><sub>DP</sub>, are better suited for estimating rain rate <i>R</i> than just the reflectivity factor for horizontally polarized waves, <i>Z</i><sub>H</sub>. A variety of physical and empirical approaches exist to estimate the rain rate from polarimetric radar observables. The relationships vary over a wide range with the location and the weather conditions. In this study, the polarimetric radar variables were simulated for S-, C- and X-band wavelengths in order to establish radar rainfall estimators for the alpine region of the form <i>R</i>(<i>K</i><sub>DP</sub>), <i>R</i>(<i>Z</i><sub>H</sub>, <i>Z</i><sub>DR</sub>), and <i>R</i>(<i>K</i><sub>DP</sub>), <i>Z</i><sub>DR</sub>. For the simulation drop size distributions of hundreds of 1-minute-rain episodes were obtained from 2D-Video-Distrometer measurements in the mountains of Styria, Austria. The sensitivity of the polarimetric variables to temperature is investigated, as well as the influence of different rain drop shape models – including recently published ones – on radar rainfall estimators. Finally it is shown how the polarimetric radar variables change with the elevation angle of the radar antenna. http://www.adv-geosci.net/16/27/2008/adgeo-16-27-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author F. Teschl
W. L. Randeu
M. Schönhuber
R. Teschl
spellingShingle F. Teschl
W. L. Randeu
M. Schönhuber
R. Teschl
Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengths
Advances in Geosciences
author_facet F. Teschl
W. L. Randeu
M. Schönhuber
R. Teschl
author_sort F. Teschl
title Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengths
title_short Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengths
title_full Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengths
title_fullStr Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengths
title_full_unstemmed Simulation of polarimetric radar variables in rain at S-, C- and X-band wavelengths
title_sort simulation of polarimetric radar variables in rain at s-, c- and x-band wavelengths
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2008-04-01
description Polarimetric radar variables of rainfall events, like differential reflectivity <i>Z</i><sub>DR</sub>, or specific differential phase <i>K</i><sub>DP</sub>, are better suited for estimating rain rate <i>R</i> than just the reflectivity factor for horizontally polarized waves, <i>Z</i><sub>H</sub>. A variety of physical and empirical approaches exist to estimate the rain rate from polarimetric radar observables. The relationships vary over a wide range with the location and the weather conditions. In this study, the polarimetric radar variables were simulated for S-, C- and X-band wavelengths in order to establish radar rainfall estimators for the alpine region of the form <i>R</i>(<i>K</i><sub>DP</sub>), <i>R</i>(<i>Z</i><sub>H</sub>, <i>Z</i><sub>DR</sub>), and <i>R</i>(<i>K</i><sub>DP</sub>), <i>Z</i><sub>DR</sub>. For the simulation drop size distributions of hundreds of 1-minute-rain episodes were obtained from 2D-Video-Distrometer measurements in the mountains of Styria, Austria. The sensitivity of the polarimetric variables to temperature is investigated, as well as the influence of different rain drop shape models – including recently published ones – on radar rainfall estimators. Finally it is shown how the polarimetric radar variables change with the elevation angle of the radar antenna.
url http://www.adv-geosci.net/16/27/2008/adgeo-16-27-2008.pdf
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AT wlrandeu simulationofpolarimetricradarvariablesinrainatscandxbandwavelengths
AT mschonhuber simulationofpolarimetricradarvariablesinrainatscandxbandwavelengths
AT rteschl simulationofpolarimetricradarvariablesinrainatscandxbandwavelengths
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