Change of extreme rainfall indexes at Ebro River Basin

Extreme rainfall events are a serious concern for regional hydrology and agriculture in the Ebro River Basin. Repeated anomalous rainfall in recent decades has had a devastating impact on this region, both socially and economically. Some studies developed in Italy and USA have shown that there is a...

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Main Authors: J. L. Valencia, A. M. Tarquis, A. Saá-Requejo, J. M. Gascó
Format: Article
Language:English
Published: Copernicus Publications 2012-07-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/12/2127/2012/nhess-12-2127-2012.pdf
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spelling doaj-624e194285a4417f96b1a98824fe3ec42020-11-24T22:44:02ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812012-07-011272127213710.5194/nhess-12-2127-2012Change of extreme rainfall indexes at Ebro River BasinJ. L. ValenciaA. M. TarquisA. Saá-RequejoJ. M. GascóExtreme rainfall events are a serious concern for regional hydrology and agriculture in the Ebro River Basin. Repeated anomalous rainfall in recent decades has had a devastating impact on this region, both socially and economically. Some studies developed in Italy and USA have shown that there is a change in seasonal patterns and an increasing frequency of extreme rainfall events, whereas other studies have pointed out that no global behaviour could be observed in monthly trends due to high climatic variability. The aim of this work is to test which of these scenarios is the case for the Ebro River Basin. <br><br> For this purpose, 14 meteorological stations were selected based on the length of the rainfall series and the climatic classification to obtain a representative untreated dataset from the river basin. Daily rainfall series from 1957 to 2002 were obtained from each meteorological station. First, classical climatic indexes were analysed with an autoregressive test to study possible trends in rainfall. The results can be explained following the evolution of the NAO and WeMO indexes, which indicate that the initial period should be subdivided in two periods (1957–1979 and 1980–2002) to assume stationarity and to analyse the rainfall distribution functions. <br><br> The general results obtained in this study for both sub-periods, through the generalised Pareto distribution (GPD) parameters and the maximum expected return values, do not support the results previously obtained by other authors that affirm a positive trend in extreme rainfall indexes and point to a slight reduction indicated by others. Three extreme precipitation indexes show negative statistical significant trends. GPD-scale parameters decrease except for only one rain gauge, although this decrease is only statistically significant for two rain gauges. Another two locations show statistical significance decreased for maximum expected return values.http://www.nat-hazards-earth-syst-sci.net/12/2127/2012/nhess-12-2127-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. L. Valencia
A. M. Tarquis
A. Saá-Requejo
J. M. Gascó
spellingShingle J. L. Valencia
A. M. Tarquis
A. Saá-Requejo
J. M. Gascó
Change of extreme rainfall indexes at Ebro River Basin
Natural Hazards and Earth System Sciences
author_facet J. L. Valencia
A. M. Tarquis
A. Saá-Requejo
J. M. Gascó
author_sort J. L. Valencia
title Change of extreme rainfall indexes at Ebro River Basin
title_short Change of extreme rainfall indexes at Ebro River Basin
title_full Change of extreme rainfall indexes at Ebro River Basin
title_fullStr Change of extreme rainfall indexes at Ebro River Basin
title_full_unstemmed Change of extreme rainfall indexes at Ebro River Basin
title_sort change of extreme rainfall indexes at ebro river basin
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2012-07-01
description Extreme rainfall events are a serious concern for regional hydrology and agriculture in the Ebro River Basin. Repeated anomalous rainfall in recent decades has had a devastating impact on this region, both socially and economically. Some studies developed in Italy and USA have shown that there is a change in seasonal patterns and an increasing frequency of extreme rainfall events, whereas other studies have pointed out that no global behaviour could be observed in monthly trends due to high climatic variability. The aim of this work is to test which of these scenarios is the case for the Ebro River Basin. <br><br> For this purpose, 14 meteorological stations were selected based on the length of the rainfall series and the climatic classification to obtain a representative untreated dataset from the river basin. Daily rainfall series from 1957 to 2002 were obtained from each meteorological station. First, classical climatic indexes were analysed with an autoregressive test to study possible trends in rainfall. The results can be explained following the evolution of the NAO and WeMO indexes, which indicate that the initial period should be subdivided in two periods (1957–1979 and 1980–2002) to assume stationarity and to analyse the rainfall distribution functions. <br><br> The general results obtained in this study for both sub-periods, through the generalised Pareto distribution (GPD) parameters and the maximum expected return values, do not support the results previously obtained by other authors that affirm a positive trend in extreme rainfall indexes and point to a slight reduction indicated by others. Three extreme precipitation indexes show negative statistical significant trends. GPD-scale parameters decrease except for only one rain gauge, although this decrease is only statistically significant for two rain gauges. Another two locations show statistical significance decreased for maximum expected return values.
url http://www.nat-hazards-earth-syst-sci.net/12/2127/2012/nhess-12-2127-2012.pdf
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