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Point to Area Rainfall Relations in the Context of Climate Change

机译:气候变化背景下的区域降雨关系

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For hydraulic structure design purposes, precipitation over an area for a specified duration and return period is commonly used in the estimation of floods. The main objective of the present paper is to propose a methodology for constructing the point-to-area rainfall relations in the context of climate change. In particular, a comparative study was carried out to assess the accuracy and reliability of the proposed method as compared to other existing methods using rainfall and climate data available from different sources in the southern Quebec and southern Alberta regions in Canada: observed daily rainfall data from rain gauges, Canadian Regional Climate Model (CRCM) output, and data given by different General Circulation Models (GCMs). The popular SDSM regression-based statistical downscaling method, the quantile-mapping, and the bias correction method were used to describe the linkage between large-scale climate variables given by the considered GCMs and local rainfall characteristics. Results of this illustrative application have indicated that the use of downscaling methods could provide the most accurate point-to-area rainfall relations as compared to the observed empirical ones, while the results given by the GCMs without downscaling and the CRCM were not accurate and displayed a very high level of uncertainty for both regions.
机译:出于水力结构设计的目的,在洪水的估计中通常使用指定持续时间和恢复期的区域内的降水量。本文的主要目的是提出一种在气候变化的背景下建立点对面降雨关系的方法。尤其是,使用从魁北克南部和加拿大艾伯塔省南部的不同来源获得的降雨和气候数据,与其他现有方法进行了比较研究,以评估该方法与其他现有方法的准确性和可靠性:观察到的每日降雨数据雨量计,加拿大区域气候模型(CRCM)输出以及不同总体循环模型(GCM)给出的数据。流行的基于SDSM回归的统计降尺度方法,分位数映射和偏差校正方法用于描述考虑的GCM给出的大规模气候变量与局部降雨特征之间的联系。该说明性应用的结果表明,与观察到的经验值相比,降尺度方法的使用可以提供最准确的点到面降雨关系,而没有降尺度的GCM和CRCM给出的结果不准确且无法显示。两个地区的不确定性都很高。

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