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Regionalization of droughts in Portugal

机译:葡萄牙干旱的区域化

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Droughts are complex natural hazards that distress large worldwide areas every year with serious impacts on society, environment and economy. Despite their importance they are still among the least understood extreme weather events. This paper is focused on the identification of regional patterns of droughts in Mainland Portugal based on monthly precipitation data, from September 1910 to October 2004, in 144 rain gages distributed uniformly over the country. The drought events were described by means of the Standardized Precipitation Index (SPI) applied to different time scales. To assess the spatial and temporal patterns of droughts, a principal component analysis (PCA) and K-means clustering method (KMC) were applied to the SPI series. The study showed that, for the different times scales, both methods resulted in an equivalent areal zoning, with three regions with different behaviours: the north, the centre and the south of Portugal. These three regions are consistent with the precipitation spatial distribution in Portugal Mainland, which in general terms decrease from North to South, with the central mountainous region representing the transition between the wet north and the progressively dry south. As the mean annual precipitation decreases southwards the hydrological regime becomes more irregular and consequently more prone to droughts.
机译:干旱是复杂的自然灾害那年与社会,环境和经济造成严重影响,困扰全球的大面积每。尽管它们的重要性,他们仍然是最不被理解极端气候事件之一。本文的重点是基于每月的降水资料在葡萄牙大陆干旱的区域格局的确定,从1910年9月至2004年10,在144个雨量计均匀分布在全国各地。干旱事件由施加到不同的时间尺度标准降水指数(SPI)来描述。为了评估干旱的空间和时间模式中,主成分分析(PCA)和K-means聚类方法(KMC)施加到SPI系列。研究表明,在不同的时间尺度,这两种方法导致了相当的面分区,有三个地区,具有不同的行为:北部,中部和葡萄牙的南部。这三个地区是在葡萄牙大陆降水量空间分布,这在一般条款从北到南减少,与代表湿北部和逐渐干燥南部之间的过渡中部山区是一致的。由于平均年降水量减少向南水文情势变得更加不规则,因此更容易出现干旱。

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