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Analysis and objective mapping of extreme daily rainfall in Catalonia

机译:加泰罗尼亚每日极端降雨的分析和客观制图

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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.
机译:这项研究的主要目的是确定在几个确定的回归期以高空间分辨率在加泰罗尼亚的最大日降水量。为此,分析了加泰罗尼亚国家气象研究所(INM)(西班牙气象局)145个测雨站的最大日降雨量年度序列。使用霍斯金(Hosking)的L矩方法,每个系列都通过Gumbel的极值分布函数进行拟合。通过这种拟合,已经确定了每个测雨站的最大日降水量,对应于2到500年之间的回归期。应用Cressman方法,已经对这些值进行了空间分析。通过应用地理信息系统(GIS)技术获得的每月降水气候数据已被用作分析的初始领域。加泰罗尼亚在1 km(2)空间分辨率上的最大日降水量已通过所采用的方法客观确定,并且可以识别出波长长于大约35 kin的结构。结果表明,预计最大日降水量的地区是横向山脉的吉列山脉地区,加泰罗尼亚州东北端的加泰罗尼亚比利牛斯​​山脉最高地区和克鲁斯角地区以及南部,沿海地区和前沿海山脉。范围在普拉德山脉和蒙西亚山脉之间。已经发现最小值的分布与最干燥的加泰罗尼亚地区之间的良好契合,最小值位于中部盆地的西端。版权所有(C)2006皇家气象学会。

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