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Copula-based risk evaluation of droughts across the Pearl River basin, China

机译:基于Copula的珠江流域干旱风险评估

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摘要

Daily precipitation data for the period of 1960-2005 from 42 precipitation gauging stations in the Pearl River basin were analyzed using the Mann-Kendall trend test and copula functions. The standardized precipitation index method was used to define drought episodes. Primary and secondary return periods were also analyzed to evaluate drought risks in the Pearl River basin as a whole. Results indicated that: (1) in general, the drought tendency was not significant at a 95 % confidence level. However, significant drought trends could be found in November, December, and January and significant wetting trends in June and July. The drought severity and drought durations were not significant at most of the precipitation stations across the Pearl River basin; (2) in terms of drought risk, higher drought risk could be observed in the lower Pearl River basin and lower drought risk in the upper Pearl River basin. Higher risk of droughts of longer durations was always corresponding to the higher risk of droughts with higher drought severity, which poses an increasing challenge for drought management and water resources management. When drought episodes with higher drought severity occurred in the Pearl River basin, the regions covered by higher risk of drought events were larger, which may challenge the water supply in the lower Pearl River basin. As for secondary return periods, results of this study indicated that secondary return periods might provide a more robust evaluation of drought risk. This study should be of merit for water resources management in the Pearl River basin, particularly the lower Pearl River basin, and can also act as a case study for determining regional response to drought changes as a result of global climate changes.
机译:利用Mann-Kendall趋势检验和copula函数分析了1960-2005年珠江流域42个测雨站的日降水量数据。标准化降水指数方法用于定义干旱发作。还对初次和二次返回期进行了分析,以评估整个珠江流域的干旱风险。结果表明:(1)一般而言,在95%的置信度下干旱趋势并不明显。但是,在11月,12月和1月会发现明显的干旱趋势,而在6月和7月会发现明显的湿润趋势。珠江流域大部分降水站的干旱严重程度和干旱持续时间均不显着。 (2)就干旱风险而言,珠江下游地区干旱风险较高,珠江上游地区干旱风险较低。持续时间较长的干旱风险总是与干旱严重程度较高的干旱风险相对应,这对干旱管理和水资源管理构成了越来越大的挑战。当珠江流域发生干旱严重程度较高的干旱事件时,受干旱事件影响更大的区域就会更大,这可能会挑战珠江下游流域的水供应。至于次要回归期,这项研究的结果表明,次要回归期可能会提供更可靠的干旱风险评估。这项研究对于珠江流域,特别是珠江下游流域的水资源管理,应该是有益的,并且也可以作为确定区域应对全球气候变化对干旱变化的反应的案例研究。

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  • 来源
    《Theoretical and applied climatology》 |2013年第2期|119-131|共13页
  • 作者单位

    Department of Water Resources and Environment, Sun Yat-sen University, Guangzhou 510275, China, Key Laboratory of Water Cycle and Water Security in Southern China of Guangdong High Education Institute, Sun Yat-sen University, Guangzhou 510275, China, School of Geography and Planning and Guangdong Key Laboratory for Urbanization and Geo-simulation, Sun Yat-sen University, Guangzhou China;

    Department of Water Resources and Environment, Sun Yat-sen University, Guangzhou 510275, China, Key Laboratory of Water Cycle and Water Security in Southern China of Guangdong High Education Institute, Sun Yat-sen University, Guangzhou 510275, China, School of Geography and Planning and Guangdong Key Laboratory for Urbanization and Geo-simulation, Sun Yat-sen University, Guangzhou China;

    Department of Biological and Agricultural Engineering and Department of Civil and Environmental Engineering, Texas A & M University, College Station TX 77843-2117, USA;

    Department of Water Resources and Environment, Sun Yat-sen University, Guangzhou 510275, China, Key Laboratory of Water Cycle and Water Security in Southern China of Guangdong High Education Institute, Sun Yat-sen University, Guangzhou 510275, China, School of Geography and Planning and Guangdong Key Laboratory for Urbanization and Geo-simulation, Sun Yat-sen University, Guangzhou China;

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