Volume 27, Issue 4
Research Article
Free Access

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

F. S. Rodrigo

Corresponding Author

E-mail address: frodrigo@ual.es

Department of Applied Physics, University of Almería, La Cañada de San Urbano, s/n, 04120 Almería, Spain

Department of Applied Physics, University of Almería, La Cañada de San Urbano, s/n, 04120 Almería, SpainSearch for more papers by this author
Ricardo M. Trigo

Centro de Geofísica da Universidades de Lisboa, Departamento de Física, Faculdade de Ciências, Universidade de Lisboa, Campo Grande, Ed C, Piso 6, 17409‐016, Lisboa, Portugal

Universidade Lusófona, Departamento de Engenharias, Lisbon, Portugal

Search for more papers by this author
First published: 09 October 2006
Citations: 122

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.

Number of times cited according to CrossRef: 122

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