Melting-layer modelling at C-Band

Stratiform cloud formations, such as a uniform type of precipitating clouds, are sub dividable into layers with different aggregate states. In this way, it is adaptable to measurements with polarimetric radar. An important task here is the detection of the transition zone between the liquid particle...

Full description

Bibliographic Details
Main Authors: J. Steinert, M. Chandra
Format: Article
Language:deu
Published: Copernicus Publications 2010-11-01
Series:Advances in Radio Science
Online Access:http://www.adv-radio-sci.net/8/285/2010/ars-8-285-2010.pdf
id doaj-2ca4782e81294b4794cef20c024425da
record_format Article
spelling doaj-2ca4782e81294b4794cef20c024425da2020-11-24T20:51:01ZdeuCopernicus PublicationsAdvances in Radio Science 1684-99651684-99732010-11-01828528810.5194/ars-8-285-2010Melting-layer modelling at C-BandJ. Steinert0M. Chandra1Professorship of Microwave Engineering and Photonics, Chemnitz University of Technology, GermanyProfessorship of Microwave Engineering and Photonics, Chemnitz University of Technology, GermanyStratiform cloud formations, such as a uniform type of precipitating clouds, are sub dividable into layers with different aggregate states. In this way, it is adaptable to measurements with polarimetric radar. An important task here is the detection of the transition zone between the liquid particles (raindrops) below and the frozen particles (ice crystals) above, i.e. the melting-layer. Linked to the physical behaviour of melting, the measured signatures, from this area, include ice crystals and raindrops in different aggregate stages. A given melting-layer model will be analysed and the comparison to models for raindrops and ice particles from earlier studies will be done. Then the results are compared with measured signatures from the C-Band radar, POLDIRAD (Oberpfaffenhofen). So we shall seek an answer to the question whether the results are sufficient to create a melting-layer-class for hydrometeor classification.http://www.adv-radio-sci.net/8/285/2010/ars-8-285-2010.pdf
collection DOAJ
language deu
format Article
sources DOAJ
author J. Steinert
M. Chandra
spellingShingle J. Steinert
M. Chandra
Melting-layer modelling at C-Band
Advances in Radio Science
author_facet J. Steinert
M. Chandra
author_sort J. Steinert
title Melting-layer modelling at C-Band
title_short Melting-layer modelling at C-Band
title_full Melting-layer modelling at C-Band
title_fullStr Melting-layer modelling at C-Band
title_full_unstemmed Melting-layer modelling at C-Band
title_sort melting-layer modelling at c-band
publisher Copernicus Publications
series Advances in Radio Science
issn 1684-9965
1684-9973
publishDate 2010-11-01
description Stratiform cloud formations, such as a uniform type of precipitating clouds, are sub dividable into layers with different aggregate states. In this way, it is adaptable to measurements with polarimetric radar. An important task here is the detection of the transition zone between the liquid particles (raindrops) below and the frozen particles (ice crystals) above, i.e. the melting-layer. Linked to the physical behaviour of melting, the measured signatures, from this area, include ice crystals and raindrops in different aggregate stages. A given melting-layer model will be analysed and the comparison to models for raindrops and ice particles from earlier studies will be done. Then the results are compared with measured signatures from the C-Band radar, POLDIRAD (Oberpfaffenhofen). So we shall seek an answer to the question whether the results are sufficient to create a melting-layer-class for hydrometeor classification.
url http://www.adv-radio-sci.net/8/285/2010/ars-8-285-2010.pdf
work_keys_str_mv AT jsteinert meltinglayermodellingatcband
AT mchandra meltinglayermodellingatcband
_version_ 1716803038456315904