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Distributions of long dry spells in the iberian peninsula, years 1951–1990
Author(s) -
Lana X.,
Martínez M. D.,
Burgueño A.,
Serra C.,
MartínVide J.,
Gómez L.
Publication year - 2006
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.1354
Subject(s) - generalized pareto distribution , skewness , kurtosis , percentile , return period , extreme value theory , climatology , generalized extreme value distribution , peninsula , series (stratigraphy) , environmental science , precipitation , gamma distribution , mathematics , statistics , meteorology , geography , geology , paleontology , archaeology , flood myth
Statistical distributions of annual extreme and long dry spells for the Iberian Peninsula are investigated by using a daily database compiled from 43 rain gauges, with the recording period extending from 1951 to 1990 and with a minor lack of data. Dry spell lengths are derived for three different daily rainfall thresholds of 0.1, 1.0 and 5.0 mm/day. On one hand, the generalised extreme value (GEV) and generalised Pareto (GP) distributions are considered for modelling the series of annual extreme (AE) dry spells. On the other hand, both theoretical distributions are assumed for the partial duration (PD) series, which are derived from the dry spell lengths exceeding the 95th percentile. In both cases, a robust estimation of the three parameters of the GEV and GP distributions is obtained by L‐moments. The fit between empirical and theoretical distributions is evaluated by using the 95% confidence bands of the Kolmogorov–Smirnov test and the L‐skewness‐kurtosis distance. Even though AE spells are quite well fitted by the GEV model, the GP distribution is a better option for some rain gauges. The PD series are usually better fitted by the GP distribution, only a few cases being better modelled by the GEV distribution. The basis for climatic drought risk assessment in the Iberian Peninsula is then established for dry spell lengths associated with return periods of 2, 5, 10, 25 and 50 years and accurately reviewed by comparing with results deduced from the AE and PD sampling strategies. As a general feature, both the spatial distribution of the statistical parameters and the dry spell lengths for the different return periods depict a north to south gradient. Some local deviations of this behaviour could be due to the vicinity to the Mediterranean Sea and the Atlantic Ocean. Copyright © 2006 Royal Meteorological Society