First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime data

A new technique for process-oriented rain area classification using Meteosat Second Generation SEVIRI nighttime data is introduced. It is based on a combination of the Advective Convective Technique (ACT) which focuses on precipitation areas connected to convective processes and the Rain Area Deline...

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Main Authors: B. Thies, T. Nauss, J. Bendix
Format: Article
Language:English
Published: Copernicus Publications 2008-04-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/16/63/2008/adgeo-16-63-2008.pdf
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spelling doaj-264a188e1d834574a8de213fd5049f0e2020-11-24T22:36:25ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592008-04-01166372First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime dataB. ThiesT. NaussJ. BendixA new technique for process-oriented rain area classification using Meteosat Second Generation SEVIRI nighttime data is introduced. It is based on a combination of the Advective Convective Technique (ACT) which focuses on precipitation areas connected to convective processes and the Rain Area Delineation Scheme during Nighttime (RADS-N) a new technique for the improved detection of stratiform precipitation areas (e.g. in connection with mid-latitude frontal systems). The ACT which uses positive brightness temperature differences between the water vapour (WV) and the infrared (IR) channels (ΔT<sub>WV-IR</sub>) for the detection of convective clouds and connected precipitating clouds has been transferred from Meteosat First Generation (MFG) Metesoat Visible and Infra-Red Imager radiometer (MVIRI) to Meteosat Second Generation (MSG) Spinning Enhanced Visible and InfraRed Imager (SEVIRI). RADS-N is based on the new conceptual model that precipitating cloud areas are characterised by a large cloud water path (<i>cwp</i>) and the presence of ice particles in the upper part of the cloud. The technique considers information about both parameters inherent in the channel differences ΔT<sub>3.9-10.8</sub>, ΔT<sub>3.9-7.3</sub>, ΔT<sub>8.7-10.8</sub>, and ΔT<sub>10.8-12.1</sub>, to detect potentially precipitating cloud areas. All four channel differences are used to gain implicit knowledge about the <i>cwp</i>. ΔT<sub>8.7-10.8</sub> and ΔT<sub>10.8-12.1</sub> are additionally considered to gain information about the cloud phase. First results of a comparison study between the classified rain areas and corresponding ground based radar data for precipitation events in connection with a cold front occlusion show encouraging performance of the new proposed process-oriented rain area classification scheme. http://www.adv-geosci.net/16/63/2008/adgeo-16-63-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. Thies
T. Nauss
J. Bendix
spellingShingle B. Thies
T. Nauss
J. Bendix
First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime data
Advances in Geosciences
author_facet B. Thies
T. Nauss
J. Bendix
author_sort B. Thies
title First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime data
title_short First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime data
title_full First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime data
title_fullStr First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime data
title_full_unstemmed First results on a process-oriented rain area classification technique using Meteosat Second Generation SEVIRI nighttime data
title_sort first results on a process-oriented rain area classification technique using meteosat second generation seviri nighttime data
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2008-04-01
description A new technique for process-oriented rain area classification using Meteosat Second Generation SEVIRI nighttime data is introduced. It is based on a combination of the Advective Convective Technique (ACT) which focuses on precipitation areas connected to convective processes and the Rain Area Delineation Scheme during Nighttime (RADS-N) a new technique for the improved detection of stratiform precipitation areas (e.g. in connection with mid-latitude frontal systems). The ACT which uses positive brightness temperature differences between the water vapour (WV) and the infrared (IR) channels (ΔT<sub>WV-IR</sub>) for the detection of convective clouds and connected precipitating clouds has been transferred from Meteosat First Generation (MFG) Metesoat Visible and Infra-Red Imager radiometer (MVIRI) to Meteosat Second Generation (MSG) Spinning Enhanced Visible and InfraRed Imager (SEVIRI). RADS-N is based on the new conceptual model that precipitating cloud areas are characterised by a large cloud water path (<i>cwp</i>) and the presence of ice particles in the upper part of the cloud. The technique considers information about both parameters inherent in the channel differences ΔT<sub>3.9-10.8</sub>, ΔT<sub>3.9-7.3</sub>, ΔT<sub>8.7-10.8</sub>, and ΔT<sub>10.8-12.1</sub>, to detect potentially precipitating cloud areas. All four channel differences are used to gain implicit knowledge about the <i>cwp</i>. ΔT<sub>8.7-10.8</sub> and ΔT<sub>10.8-12.1</sub> are additionally considered to gain information about the cloud phase. First results of a comparison study between the classified rain areas and corresponding ground based radar data for precipitation events in connection with a cold front occlusion show encouraging performance of the new proposed process-oriented rain area classification scheme.
url http://www.adv-geosci.net/16/63/2008/adgeo-16-63-2008.pdf
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