%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Hammami, Hela
%A Carreau, Julie
%A Neppel, L.
%A Elasmi, S.
%A Feki, H.
%T Smooth spatial modeling of extreme Mediterranean precipitation
%D 2022
%L fdi:010086666
%G ENG
%J Water
%K intense precipitation events ; non-stationarity in space ; generalized ; extreme value distribution ; spatial interpolation ; generalized linear ; models ; artificial neural networks
%K TUNISIE ; ZONE MEDITERRANEENNE
%M ISI:000887786100001
%N 22
%P 3782 [18 ]
%R 10.3390/w14223782
%U https://www.documentation.ird.fr/hor/fdi:010086666
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/2023-01/010086666.pdf
%V 14
%W Horizon (IRD)
%X Extreme precipitation events can lead to disastrous floods, which are the most significant natural hazards in the Mediterranean regions. Therefore, a proper characterization of these events is crucial. Extreme events defined as annual maxima can be modeled with the generalized extreme value (GEV) distribution. Owing to spatial heterogeneity, the distribution of extremes is non-stationary in space. To take non-stationarity into account, the parameters of the GEV distribution can be viewed as functions of covariates that convey spatial information. Such functions may be implemented as a generalized linear model (GLM) or with a more flexible non-parametric non-linear model such as an artificial neural network (ANN). In this work, we evaluate several statistical models that combine the GEV distribution with a GLM or with an ANN for a spatial interpolation of the GEV parameters. Key issues are the proper selection of the complexity level of the ANN (i.e., the number of hidden units) and the proper selection of spatial covariates. Three sites are included in our study: a region in the French Mediterranean, the Cap Bon area in northeast Tunisia, and the Merguellil catchment in central Tunisia. The comparative analysis aim at assessing the genericity of state-of-the-art approaches to interpolate the distribution of extreme precipitation events.
%$ 062 ; 020 ; 021