Impact of integration time steps of rain drop size distribution on their double-moment normalization: a case study in northern Benin

This study analyzed the sensitivity of the double-moment normalization of rain drop size distributions (DSDs) to their integration time steps. Six DSD datasets measured at different integration time steps were modeled by the double-moment normalization method. Six couples of reference moments are us...

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Main Authors: Moumouni, Sounmaïla, Akponi, Fulgence Payot, Zahiri, Eric-Pascal, Lawin, Agnidé Emmanuel, Gosset, Marielle
Format: Article
Language:English
Published: Académie des sciences 2023-02-01
Series:Comptes Rendus. Géoscience
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Online Access:https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.200/
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author Moumouni, Sounmaïla
Akponi, Fulgence Payot
Zahiri, Eric-Pascal
Lawin, Agnidé Emmanuel
Gosset, Marielle
author_facet Moumouni, Sounmaïla
Akponi, Fulgence Payot
Zahiri, Eric-Pascal
Lawin, Agnidé Emmanuel
Gosset, Marielle
author_sort Moumouni, Sounmaïla
collection DOAJ
description This study analyzed the sensitivity of the double-moment normalization of rain drop size distributions (DSDs) to their integration time steps. Six DSD datasets measured at different integration time steps were modeled by the double-moment normalization method. Six couples of reference moments are used for the normalization. Three DSD models (gamma, generalized gamma and lognormal) are used for modeling. Statistical criteria are used to assess the estimation of the moments of the DSDs made by the models. As results, the analysis highlighted the dependence of the shape function parameters on the DSD integration time step. It is also noted that the three DSD models are well adapted to the data used. Nevertheless, the generalized gamma model is recommended because of the independence of the moment estimation errors with respect to the integration time step, which is not the case for the other models.
format Article
id doaj-art-f35018b7e21e487288e8ba46cc7e4264
institution Kabale University
issn 1778-7025
language English
publishDate 2023-02-01
publisher Académie des sciences
record_format Article
series Comptes Rendus. Géoscience
spelling doaj-art-f35018b7e21e487288e8ba46cc7e42642025-02-07T10:39:55ZengAcadémie des sciencesComptes Rendus. Géoscience1778-70252023-02-01355G110913310.5802/crgeos.20010.5802/crgeos.200Impact of integration time steps of rain drop size distribution on their double-moment normalization: a case study in northern BeninMoumouni, Sounmaïla0https://orcid.org/0000-0001-6451-2169Akponi, Fulgence Payot1https://orcid.org/0000-0002-7736-2371Zahiri, Eric-Pascal2https://orcid.org/0000-0003-0536-1764Lawin, Agnidé Emmanuel3https://orcid.org/0000-0003-4751-3439Gosset, Marielle4https://orcid.org/0000-0003-1064-7003Ecole Normale Supérieure (ENS) de Natitingou, Université Nationale des Sciences, Technologies, Ingénierie et Mathématiques (UNSTIM), BéninDépartement Physique, Faculté des Sciences et Techniques; Université d’Abomey-Calavi, Bénin; Ecole Normale Supérieure (ENS) de Natitingou, Université Nationale des Sciences, Technologies, Ingénierie et Mathématiques (UNSTIM), BéninLaboratoire des Sciences de la Matière, de l’Environnement et de l’Energie Solaire, Université Félix Houphouët-Boigny, Côte d’IvoireLaboratoire d’Hydrologie Appliquée (LHA), Institut National de l’Eau (INE), Université d’Abomey-Calavi, BeninGéosciences-Environnement-Toulouse (GET), Institut de Recherche pour le Développement (IRD), FranceThis study analyzed the sensitivity of the double-moment normalization of rain drop size distributions (DSDs) to their integration time steps. Six DSD datasets measured at different integration time steps were modeled by the double-moment normalization method. Six couples of reference moments are used for the normalization. Three DSD models (gamma, generalized gamma and lognormal) are used for modeling. Statistical criteria are used to assess the estimation of the moments of the DSDs made by the models. As results, the analysis highlighted the dependence of the shape function parameters on the DSD integration time step. It is also noted that the three DSD models are well adapted to the data used. Nevertheless, the generalized gamma model is recommended because of the independence of the moment estimation errors with respect to the integration time step, which is not the case for the other models.https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.200/Rain DSDDouble-moment normalizationIntegration time stepsUnimodal DSD modelsGeneralized gammaWeather radarsWest Africa rainfall
spellingShingle Moumouni, Sounmaïla
Akponi, Fulgence Payot
Zahiri, Eric-Pascal
Lawin, Agnidé Emmanuel
Gosset, Marielle
Impact of integration time steps of rain drop size distribution on their double-moment normalization: a case study in northern Benin
Comptes Rendus. Géoscience
Rain DSD
Double-moment normalization
Integration time steps
Unimodal DSD models
Generalized gamma
Weather radars
West Africa rainfall
title Impact of integration time steps of rain drop size distribution on their double-moment normalization: a case study in northern Benin
title_full Impact of integration time steps of rain drop size distribution on their double-moment normalization: a case study in northern Benin
title_fullStr Impact of integration time steps of rain drop size distribution on their double-moment normalization: a case study in northern Benin
title_full_unstemmed Impact of integration time steps of rain drop size distribution on their double-moment normalization: a case study in northern Benin
title_short Impact of integration time steps of rain drop size distribution on their double-moment normalization: a case study in northern Benin
title_sort impact of integration time steps of rain drop size distribution on their double moment normalization a case study in northern benin
topic Rain DSD
Double-moment normalization
Integration time steps
Unimodal DSD models
Generalized gamma
Weather radars
West Africa rainfall
url https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.200/
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