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Copula-based probabilistic characterization of precipitation extremes over North Sikkim Himalaya

机译:北锡金喜马拉雅山极端降水的基于Copula的概率表征

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Changes in climate extremes are studied based on the daily precipitation in North Sikkim Himalaya. The Coupled Model Intercomparison Project Phase 5 (CMIP5) Global Climate Models GCMs) and their Representative Concentration Pathways (RCPs) and India Meteorological Department (IMD) daily precipitation dataset are used for future and observed time periods, respectively. The purpose of this study is to examine the copula-based probabilistic behavior of precipitation extremes over the eastern Himalayan region. Seven extreme combinations were developed based on the eight defined precipitation indices. The extreme combination designates the duration, frequency and amount of heavy and weak precipitation in the same year. Statistical downscaling model (SDSM) and copulas are used for downscaling and bivariate behavior of precipitation extremes, respectively. Trend analysis result exhibits that the precipitation and its extremes (intensity, wet days, heavy precipitation days and very heavy precipitation days) are increasing significantly during 2006-2100. The spatial distributions of joint return period (JRP) of (T5, T10 and T20) marginal values are quite same during 1979-2005. In addition, the co-occurrences of heavy and weak precipitation would be more frequent in future, resulting higher risk of floods and droughts within the same year. The North Sikkim region may be at high risk of floods because precipitation extremes are increasing along with co-occurrence of flood and drought in the same year.
机译:根据北锡金喜马拉雅山的每日降水量研究了极端气候的变化。耦合模型比较项目第5阶段(CMIP5)全球气候模型GCM)及其代表浓度路径(RCP)和印度气象局(IMD)的日降水量数据集分别用于未来和观察到的时间段。这项研究的目的是研究喜马拉雅东部地区极端降水的基于copula的概率行为。根据八个定义的降水指数开发了七个极端组合。极端组合表示同一年的强降水和弱降水的持续时间,频率和数量。统计降尺度模型(SDSM)和copulas分别用于极端降水的降尺度和双变量行为。趋势分析结果表明,2006-2100年期间,降水及其极端值(强度,湿日,重降水日和非常重降水日)显着增加。 (T5,T10和T20)边际值的联合返回期(JRP)的空间分布在1979-2005年期间是相同的。此外,未来强降雨和弱降雨并存的情况会更加频繁,导致同一年发生水灾和干旱的风险更高。锡金北部地区可能会发生洪灾的高风险,因为同一年洪水和干旱的共同发生使极端降水增加。

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