PM-GCD – a combined IR–MW satellite technique for frequent retrieval of heavy precipitation

Precipitation retrievals based on measurements from microwave (MW) radiometers onboard low-Earth-orbit (LEO) satellites can reach high level of accuracy – especially regarding convective precipitation. At the present stage though, these observations cannot provide satisfactory coverage of the evolut...

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Main Authors: D. Casella, S. Dietrich, F. Di Paola, M. Formenton, A. Mugnai, F. Porcù, P. Sanò
Format: Article
Language:English
Published: Copernicus Publications 2012-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/12/231/2012/nhess-12-231-2012.pdf
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author D. Casella
S. Dietrich
F. Di Paola
M. Formenton
A. Mugnai
F. Porcù
P. Sanò
author_facet D. Casella
S. Dietrich
F. Di Paola
M. Formenton
A. Mugnai
F. Porcù
P. Sanò
author_sort D. Casella
collection DOAJ
description Precipitation retrievals based on measurements from microwave (MW) radiometers onboard low-Earth-orbit (LEO) satellites can reach high level of accuracy – especially regarding convective precipitation. At the present stage though, these observations cannot provide satisfactory coverage of the evolution of intense and rapid precipitating systems. As a result, the obtained precipitation retrievals are often of limited use for many important applications – especially in supporting authorities for flood alerts and weather warnings. To tackle this problem, over the past two decades several techniques have been developed combining accurate MW estimates with frequent infrared (IR) observations from geosynchronous (GEO) satellites, such as the European Meteosat Second Generation (MSG). In this framework, we have developed a new fast and simple precipitation retrieval technique which we call Passive Microwave – Global Convective Diagnostic, (PM-GCD). This method uses MW retrievals in conjunction with the Global Convective Diagnostic (GCD) technique which discriminates deep convective clouds based on the difference between the MSG water vapor (6.2 μm) and thermal-IR (10.8 μm) channels. Specifically, MSG observations and the GCD technique are used to identify deep convective areas. These areas are then calibrated using MW precipitation estimates based on observations from the Advanced Microwave Sounding Unit (AMSU) radiometers onboard operational NOAA and Eumetsat satellites, and then finally propagated in time with a simple tracking algorithm. In this paper, we describe the PM-GCD technique, analyzing its results for a case study that refers to a flood event that struck the island of Sicily in southern Italy on 1–2 October 2009.
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spelling doaj.art-5017a6c271704fd78c0e318ca93362a02022-12-22T00:43:12ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812012-01-0112123124010.5194/nhess-12-231-2012PM-GCD – a combined IR–MW satellite technique for frequent retrieval of heavy precipitationD. CasellaS. DietrichF. Di PaolaM. FormentonA. MugnaiF. PorcùP. SanòPrecipitation retrievals based on measurements from microwave (MW) radiometers onboard low-Earth-orbit (LEO) satellites can reach high level of accuracy – especially regarding convective precipitation. At the present stage though, these observations cannot provide satisfactory coverage of the evolution of intense and rapid precipitating systems. As a result, the obtained precipitation retrievals are often of limited use for many important applications – especially in supporting authorities for flood alerts and weather warnings. To tackle this problem, over the past two decades several techniques have been developed combining accurate MW estimates with frequent infrared (IR) observations from geosynchronous (GEO) satellites, such as the European Meteosat Second Generation (MSG). In this framework, we have developed a new fast and simple precipitation retrieval technique which we call Passive Microwave – Global Convective Diagnostic, (PM-GCD). This method uses MW retrievals in conjunction with the Global Convective Diagnostic (GCD) technique which discriminates deep convective clouds based on the difference between the MSG water vapor (6.2 μm) and thermal-IR (10.8 μm) channels. Specifically, MSG observations and the GCD technique are used to identify deep convective areas. These areas are then calibrated using MW precipitation estimates based on observations from the Advanced Microwave Sounding Unit (AMSU) radiometers onboard operational NOAA and Eumetsat satellites, and then finally propagated in time with a simple tracking algorithm. In this paper, we describe the PM-GCD technique, analyzing its results for a case study that refers to a flood event that struck the island of Sicily in southern Italy on 1–2 October 2009.http://www.nat-hazards-earth-syst-sci.net/12/231/2012/nhess-12-231-2012.pdf
spellingShingle D. Casella
S. Dietrich
F. Di Paola
M. Formenton
A. Mugnai
F. Porcù
P. Sanò
PM-GCD – a combined IR–MW satellite technique for frequent retrieval of heavy precipitation
Natural Hazards and Earth System Sciences
title PM-GCD – a combined IR–MW satellite technique for frequent retrieval of heavy precipitation
title_full PM-GCD – a combined IR–MW satellite technique for frequent retrieval of heavy precipitation
title_fullStr PM-GCD – a combined IR–MW satellite technique for frequent retrieval of heavy precipitation
title_full_unstemmed PM-GCD – a combined IR–MW satellite technique for frequent retrieval of heavy precipitation
title_short PM-GCD – a combined IR–MW satellite technique for frequent retrieval of heavy precipitation
title_sort pm gcd a combined ir mw satellite technique for frequent retrieval of heavy precipitation
url http://www.nat-hazards-earth-syst-sci.net/12/231/2012/nhess-12-231-2012.pdf
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