Analysis and objective mapping of extreme daily rainfall in Catalonia

被引:36
作者
Casas, M. Carmen
Herrero, Monica
Ninyerola, Miquel
Pons, Xavier
Rodriguez, Rauel
Rius, Anna
Redano, Angel
机构
[1] Univ Barcelona, Dept Astron & Meteorol, E-08028 Barcelona, Spain
[2] Univ Politecn Cataluna, EPSEVG, Dept Phys & Nucl Engn, Vilanova I La Geltru 08800, Spain
[3] Gen Catalunya Berlin, Serv Meteorol Catalunya, Barcelona 08029, Spain
[4] Autonomous Univ Barcelona, Dept Anim Biol Vegetal Biol & Ecol, Unit Bot, Bellaterra 08193, Spain
[5] Autonomous Univ Barcelona, Dept Geog, Bellaterra 08193, Spain
[6] Autonomous Univ Barcelona, Ctr Ecol Res & Forestry Applicat, Bellaterra 08193, Spain
关键词
maximum daily precipitation; extreme distributions; region rainfall distribution; objective analysis technique;
D O I
10.1002/joc.1402
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The main objective of this study is to determine the maximum daily precipitation in Catalonia for several established return periods with a high spatial resolution. For this purpose, the maximum daily rainfall annual series from 145 pluviometric stations of the Instituto Nacional de Meteorologia (INM) (Spanish Weather Service) in Catalonia have been analyzed. Using the L-moments method of Hosking, every series has been fitted by the extreme value distribution function of Gumbel. From this fitting, the maximum daily precipitation for each of the pluviometric stations corresponding to return periods between 2 and 500 years, have been determined. Applying the Cressman method, the spatial analysis of these values has been achieved. Monthly precipitation climatological data, obtained from the application of Geographic Information Systems (GIS) techniques, have been used as the initial field for the analysis. The maximum daily precipitation at 1 km(2) spatial resolution on Catalonia has been objectively determined by the method employed, and structures with wavelength longer than approximately 35 kin can be identified. The results show that places where the maximum daily precipitation values are expected are the zone of Guilleries in the Transversal Range, in the highest zones of the Catalan Pyrenees and Cape Creus zone at the northeastern end of Catalonia and in the south, around the Prelittoral Mountain Range between the Mountains of Prades and Montsia. A good fit between the distribution of minimum values and the driest Catalan areas has been found, the lowest values being on the western end of the Central Basin. Copyright (C) 2006 Royal Meteorological Society.
引用
收藏
页码:399 / 409
页数:11
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