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Spatiotemporal Characteristics of Meteorological Drought for the Island of Crete

机译:克里特岛气象干旱的时空特征

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A modified drought index, named the spatially normalized-standardized precipitation index (SN-SPI), has been developed for assessing meteorological droughts. The SN-SPI is a variant index to the standardized precipitation index and is based on the probability of precipitation at different time scales, but it is spatially normalized for improved assessment of drought severity. Results of this index incorporate the spatial distribution of precipitation and produce improved drought warnings. This index is applied in the island of Crete, Greece, and the drought results are compared to the ones of SPI. A 30-year-long average monthly precipitation dataset from 130 watersheds of the island is used by the above indices for drought classification in terms of its duration and intensity. Bias-adjusted monthly precipitation estimates from an ensemble of 10 regional climate models were used to quantify the influence of global warming to drought conditions over the period 2010-2100. Results based on both indices (calculated for three time scales of 12, 24, and 48 months) from 3 basins in west, central, and east parts of the island show that 1) the extreme drought periods are the same (reaching 7% of time) but the intensities based on SN-SPI are lower; 2) the area covered by extreme droughts is 3% (first time scale), 16% (second time scale), and 25% (third time scale), and 96% (first time scale), 95% (second time scale), and 80% (third time scale) based on the SN-SPI and SPI, respectively; 3) concerning the longest time scale (48 months), more than half of the area of Crete is about to experience drought conditions during 28%, 69%, and 97% for 2010-40, 2040-70, and 2070-2100, respectively; and 4) extremely dry conditions will cover 52%, 33%, and 25% of the island for the future 90-year period using 12-, 24-, and 48-month SN-SPI, respectively.
机译:已开发出一种经修改的干旱指数,称为空间归一化标准化降水指数(SN-SPI),用于评估气象干旱。 SN-SPI是标准降水指数的变体指数,它基于不同时间尺度上的降水概率,但是为了提高对干旱严重性的评估,对空间进行了标准化。该指数的结果纳入了降水的空间分布,并产生了改善的干旱预警。该指数适用于希腊克里特岛,并将干旱结果与SPI进行了比较。上述指标使用了该岛130个流域的30年平均月降水量数据集,根据其持续时间和强度,将其用于干旱分类。使用由10个区域气候模型组成的集合进行偏差调整后的每月降水量估算,以量化2010-2100年期间全球变暖对干旱条件的影响。根据该岛西部,中部和东部三个盆地的两个指数(以三个时间尺度分别为12、24和48个月计算)得出的结果表明,1)极端干旱时期是相同的(达到7%)。时间),但基于SN-SPI的强度较低; 2)极端干旱所覆盖的区域是3%(第一时间范围),16%(第二时间范围)和25%(第三时间范围)以及96%(第一时间范围)和95%(第二时间范围) ,以及分别基于SN-SPI和SPI的80%(第三时间标度); 3)关于最长的时间尺度(48个月),克里特岛超过一半的地区在2010-40、2040-70和2070-2100期间将经历28%,69%和97%的干旱,分别;和4)在未来90年期间,极端干旱条件将分别使用12个月,24个月和48个月的SN-SPI覆盖该岛的52%,33%和25%。

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