Spatial dependences among precipitation maxima over Belgium

For a wide range of applications in hydrology, the probability distribution of precipitation maxima represents a fundamental quantity to build dykes, propose flood planning policies, or more generally, to mitigate the impact of precipitation extremes. Classical Extreme Value Theory (EVT) has been ap...

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Main Authors: S. Vannitsem, P. Naveau
Format: Article
Language:English
Published: Copernicus Publications 2007-09-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/14/621/2007/npg-14-621-2007.pdf
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spelling doaj-5c218845ffd94fd986b8e0f9b48243192020-11-25T02:16:50ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462007-09-01145621630Spatial dependences among precipitation maxima over BelgiumS. VannitsemP. NaveauFor a wide range of applications in hydrology, the probability distribution of precipitation maxima represents a fundamental quantity to build dykes, propose flood planning policies, or more generally, to mitigate the impact of precipitation extremes. Classical Extreme Value Theory (EVT) has been applied in this context by usually assuming that precipitation maxima can be considered as Independent and Identically Distributed (IID) events, which approximately follow a Generalized Extreme Value distribution (GEV) at each recording site. In practice, weather stations records can not be considered as independent in space. <br><br> Assessing the spatial dependences among precipitation maxima provided by two Belgium measurement networks is the main goal of this work. The pairwise dependences are estimated by a variogram of order one, also called madogram, that is specially tailored to be in compliance with spatial EVT and to capture EVT bivariate structures. Our analysis of Belgium precipitation maxima indicates that the degree of dependence varies greatly according to three factors: the distance between two stations, the season (summer or winter) and the precipitation accumulation duration (hourly, daily, monthly, etc.). Increasing the duration (from one hour to 20 days) strengthens the spatial dependence. The full independence is reached after about 50 km (100 km) for summer (winter) for a duration of one hour, while for long durations only after a few hundred kilometers. In addition this dependence is always larger in winter than in summer whatever is the duration. An explanation of these properties in terms of the dynamical processes dominating during the two seasons is advanced. http://www.nonlin-processes-geophys.net/14/621/2007/npg-14-621-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Vannitsem
P. Naveau
spellingShingle S. Vannitsem
P. Naveau
Spatial dependences among precipitation maxima over Belgium
Nonlinear Processes in Geophysics
author_facet S. Vannitsem
P. Naveau
author_sort S. Vannitsem
title Spatial dependences among precipitation maxima over Belgium
title_short Spatial dependences among precipitation maxima over Belgium
title_full Spatial dependences among precipitation maxima over Belgium
title_fullStr Spatial dependences among precipitation maxima over Belgium
title_full_unstemmed Spatial dependences among precipitation maxima over Belgium
title_sort spatial dependences among precipitation maxima over belgium
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2007-09-01
description For a wide range of applications in hydrology, the probability distribution of precipitation maxima represents a fundamental quantity to build dykes, propose flood planning policies, or more generally, to mitigate the impact of precipitation extremes. Classical Extreme Value Theory (EVT) has been applied in this context by usually assuming that precipitation maxima can be considered as Independent and Identically Distributed (IID) events, which approximately follow a Generalized Extreme Value distribution (GEV) at each recording site. In practice, weather stations records can not be considered as independent in space. <br><br> Assessing the spatial dependences among precipitation maxima provided by two Belgium measurement networks is the main goal of this work. The pairwise dependences are estimated by a variogram of order one, also called madogram, that is specially tailored to be in compliance with spatial EVT and to capture EVT bivariate structures. Our analysis of Belgium precipitation maxima indicates that the degree of dependence varies greatly according to three factors: the distance between two stations, the season (summer or winter) and the precipitation accumulation duration (hourly, daily, monthly, etc.). Increasing the duration (from one hour to 20 days) strengthens the spatial dependence. The full independence is reached after about 50 km (100 km) for summer (winter) for a duration of one hour, while for long durations only after a few hundred kilometers. In addition this dependence is always larger in winter than in summer whatever is the duration. An explanation of these properties in terms of the dynamical processes dominating during the two seasons is advanced.
url http://www.nonlin-processes-geophys.net/14/621/2007/npg-14-621-2007.pdf
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