Cloud physical properties and empirical polarimetric measurements of rain signatures at C-Band

Raindrops are one type of precipitation in stratiform and convective clouds. To get relationships for describing the raindrops two different methods were used. In the first way, the microphysical properties of the liquid hydrometeors were examined. For this the use of the Rayleigh approximation for...

Full description

Bibliographic Details
Main Authors: J. Steinert, M. Chandra
Format: Article
Language:deu
Published: Copernicus Publications 2008-05-01
Series:Advances in Radio Science
Online Access:http://www.adv-radio-sci.net/6/315/2008/ars-6-315-2008.pdf
id doaj-fbcbc9d4251143aba51bd03be29ea79b
record_format Article
spelling doaj-fbcbc9d4251143aba51bd03be29ea79b2020-11-25T02:16:53ZdeuCopernicus PublicationsAdvances in Radio Science 1684-99651684-99732008-05-016315318Cloud physical properties and empirical polarimetric measurements of rain signatures at C-BandJ. SteinertM. ChandraRaindrops are one type of precipitation in stratiform and convective clouds. To get relationships for describing the raindrops two different methods were used. In the first way, the microphysical properties of the liquid hydrometeors were examined. For this the use of the Rayleigh approximation for small particles (raindrops at C-Band) and the drop size distribution by Ulbrich (Γ-DSD) lead to the calculation of the reflectivity at horizontal polarisation <i>Z<sub>HH</sub></i>, the reflectivity at vertical polarisation <i>Z<sub>VV</sub></i> and the differential reflectivity <i>Z<sub>DR</sub></i>. In the second way, rain signatures were separated from polarimetric measurements. The database of these measurements consists of datasets measured by the dual polarimetric C-Band weather radar POLDIRAD (DLR, Oberpfaffenhofen). The aim of this study was then to combine and to compare the results from the real radar measurements against the theoretical calculations in the <i>Z<sub>HH</sub>-Z<sub>DR</sub></i> plane. Based on these observations and calculations, scientific results for future practical use will be presented in form of empirical equations including <i>Z<sub>HH</sub>-Z<sub>DR</sub></i>. Finally in form of scientific discussion, the <i>Z<sub>HH</sub>-Z<sub>DR</sub></i> plane will be critically assessed for outstanding problems or issues. http://www.adv-radio-sci.net/6/315/2008/ars-6-315-2008.pdf
collection DOAJ
language deu
format Article
sources DOAJ
author J. Steinert
M. Chandra
spellingShingle J. Steinert
M. Chandra
Cloud physical properties and empirical polarimetric measurements of rain signatures at C-Band
Advances in Radio Science
author_facet J. Steinert
M. Chandra
author_sort J. Steinert
title Cloud physical properties and empirical polarimetric measurements of rain signatures at C-Band
title_short Cloud physical properties and empirical polarimetric measurements of rain signatures at C-Band
title_full Cloud physical properties and empirical polarimetric measurements of rain signatures at C-Band
title_fullStr Cloud physical properties and empirical polarimetric measurements of rain signatures at C-Band
title_full_unstemmed Cloud physical properties and empirical polarimetric measurements of rain signatures at C-Band
title_sort cloud physical properties and empirical polarimetric measurements of rain signatures at c-band
publisher Copernicus Publications
series Advances in Radio Science
issn 1684-9965
1684-9973
publishDate 2008-05-01
description Raindrops are one type of precipitation in stratiform and convective clouds. To get relationships for describing the raindrops two different methods were used. In the first way, the microphysical properties of the liquid hydrometeors were examined. For this the use of the Rayleigh approximation for small particles (raindrops at C-Band) and the drop size distribution by Ulbrich (Γ-DSD) lead to the calculation of the reflectivity at horizontal polarisation <i>Z<sub>HH</sub></i>, the reflectivity at vertical polarisation <i>Z<sub>VV</sub></i> and the differential reflectivity <i>Z<sub>DR</sub></i>. In the second way, rain signatures were separated from polarimetric measurements. The database of these measurements consists of datasets measured by the dual polarimetric C-Band weather radar POLDIRAD (DLR, Oberpfaffenhofen). The aim of this study was then to combine and to compare the results from the real radar measurements against the theoretical calculations in the <i>Z<sub>HH</sub>-Z<sub>DR</sub></i> plane. Based on these observations and calculations, scientific results for future practical use will be presented in form of empirical equations including <i>Z<sub>HH</sub>-Z<sub>DR</sub></i>. Finally in form of scientific discussion, the <i>Z<sub>HH</sub>-Z<sub>DR</sub></i> plane will be critically assessed for outstanding problems or issues.
url http://www.adv-radio-sci.net/6/315/2008/ars-6-315-2008.pdf
work_keys_str_mv AT jsteinert cloudphysicalpropertiesandempiricalpolarimetricmeasurementsofrainsignaturesatcband
AT mchandra cloudphysicalpropertiesandempiricalpolarimetricmeasurementsofrainsignaturesatcband
_version_ 1724888404740538368