Trends in daily rainfall in the Iberian Peninsula from 1951 to 2002

Abstract An analysis of 22 sites of daily precipitation records over the period 1951–2002 for the Iberian Peninsula is presented. Annual and seasonal total precipitation ( P ), number of wet days ( N ), precipitation intensity ( I ), the 95th percentile ( P 95), and percentage of rain falling on day...

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Published in:International Journal of Climatology
Main Authors: Rodrigo, F. S., Trigo, Ricardo M.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2006
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.1409
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spelling crwiley:10.1002/joc.1409 2024-09-15T18:23:48+00:00 Trends in daily rainfall in the Iberian Peninsula from 1951 to 2002 Rodrigo, F. S. Trigo, Ricardo M. 2006 http://dx.doi.org/10.1002/joc.1409 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1409 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1409 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 27, issue 4, page 513-529 ISSN 0899-8418 1097-0088 journal-article 2006 crwiley https://doi.org/10.1002/joc.1409 2024-08-27T04:30:52Z Abstract An analysis of 22 sites of daily precipitation records over the period 1951–2002 for the Iberian Peninsula is presented. Annual and seasonal total precipitation ( P ), number of wet days ( N ), precipitation intensity ( I ), the 95th percentile ( P 95), and percentage of rain falling on days with rainfall above the 95th percentile (%) are investigated. The annual and seasonal trends for these variables and for all 22 rain gauges are analysed, using the Mann–Kendall statistic, and a linear regression model. Moreover, a t ‐test is applied to the difference between the means of two subperiods, respectively 1951–1976 and 1977–2002. Principal results indicate a decreasing trend in P , I , and P 95 for several northern and southern stations in winter; P , I , and P 95 in some southern stations in spring, I and P 95 in some southern stations in summer, and I in some northern and southern stations in autumn. The general behaviour is a decrease in the daily intensity of rainfall, while the number of wet days does not reveal pronounced changes. This pattern is valid for both annual and seasonal values of the indices. The decreasing trend found for I in winter and annual series for some localities may be related to the predominance of the positive phase of the North Atlantic Oscillation (NAO), but it is necessary to find other mechanisms for those stations and seasons not linked directly to NAO. Copyright © 2006 Royal Meteorological Society. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library International Journal of Climatology 27 4 513 529
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract An analysis of 22 sites of daily precipitation records over the period 1951–2002 for the Iberian Peninsula is presented. Annual and seasonal total precipitation ( P ), number of wet days ( N ), precipitation intensity ( I ), the 95th percentile ( P 95), and percentage of rain falling on days with rainfall above the 95th percentile (%) are investigated. The annual and seasonal trends for these variables and for all 22 rain gauges are analysed, using the Mann–Kendall statistic, and a linear regression model. Moreover, a t ‐test is applied to the difference between the means of two subperiods, respectively 1951–1976 and 1977–2002. Principal results indicate a decreasing trend in P , I , and P 95 for several northern and southern stations in winter; P , I , and P 95 in some southern stations in spring, I and P 95 in some southern stations in summer, and I in some northern and southern stations in autumn. The general behaviour is a decrease in the daily intensity of rainfall, while the number of wet days does not reveal pronounced changes. This pattern is valid for both annual and seasonal values of the indices. The decreasing trend found for I in winter and annual series for some localities may be related to the predominance of the positive phase of the North Atlantic Oscillation (NAO), but it is necessary to find other mechanisms for those stations and seasons not linked directly to NAO. Copyright © 2006 Royal Meteorological Society.
format Article in Journal/Newspaper
author Rodrigo, F. S.
Trigo, Ricardo M.
spellingShingle Rodrigo, F. S.
Trigo, Ricardo M.
Trends in daily rainfall in the Iberian Peninsula from 1951 to 2002
author_facet Rodrigo, F. S.
Trigo, Ricardo M.
author_sort Rodrigo, F. S.
title Trends in daily rainfall in the Iberian Peninsula from 1951 to 2002
title_short Trends in daily rainfall in the Iberian Peninsula from 1951 to 2002
title_full Trends in daily rainfall in the Iberian Peninsula from 1951 to 2002
title_fullStr Trends in daily rainfall in the Iberian Peninsula from 1951 to 2002
title_full_unstemmed Trends in daily rainfall in the Iberian Peninsula from 1951 to 2002
title_sort trends in daily rainfall in the iberian peninsula from 1951 to 2002
publisher Wiley
publishDate 2006
url http://dx.doi.org/10.1002/joc.1409
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1409
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1409
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source International Journal of Climatology
volume 27, issue 4, page 513-529
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.1409
container_title International Journal of Climatology
container_volume 27
container_issue 4
container_start_page 513
op_container_end_page 529
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