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使用网格化日降雨数据作为协变量对短历时极端降雨进行区域频率分析。

Regional frequency analysis of short duration rainfall extremes using gridded daily rainfall data as co-variate.

作者信息

Madsen H, Gregersen I B, Rosbjerg D, Arnbjerg-Nielsen K

机构信息

DHI, Agern Allé 5, DK-2970 Hørsholm, Denmark E-mail:

Department of Environmental Engineering, Technical University of Denmark, Bygningstorvet Building 115, DK-2800 Kgs. Lyngby, Denmark.

出版信息

Water Sci Technol. 2017 Apr;75(7-8):1971-1981. doi: 10.2166/wst.2017.089.

DOI:10.2166/wst.2017.089
PMID:28452789
Abstract

A regional partial duration series (PDS) model is applied for estimation of intensity duration frequency relationships of extreme rainfalls in Denmark. The model uses generalised least squares regression to relate the PDS parameters to gridded rainfall statistics from a dense network of rain gauges with daily measurements. The Poisson rate is positively correlated to the mean annual precipitation for all durations considered (1 min to 48 hours). The mean intensity can be assumed constant over Denmark for durations up to 1 hour. For durations larger than 1 hour, the mean intensity is significantly correlated to the mean extreme daily precipitation. A Generalised Pareto distribution with a regional constant shape parameter is adopted. Compared to previous regional studies in Denmark, a general increase in extreme rainfall intensity for durations up to 1 hour is found, whereas for larger durations both increases and decreases are seen. A subsample analysis is conducted to evaluate the impacts of non-stationarities in the rainfall data. The regional model includes the non-stationarities as an additional source of uncertainty, together with sampling uncertainty and uncertainty caused by spatial variability.

摘要

应用区域部分历时序列(PDS)模型来估算丹麦极端降雨的强度-历时-频率关系。该模型使用广义最小二乘回归,将PDS参数与来自具有日测量数据的密集雨量计网络的网格化降雨统计数据相关联。对于所有考虑的历时(1分钟至48小时),泊松率与年平均降水量呈正相关。对于历时长达1小时的情况,可以假设丹麦各地的平均强度是恒定的。对于历时大于1小时的情况,平均强度与极端日降水量均值显著相关。采用具有区域恒定形状参数的广义帕累托分布。与丹麦以前的区域研究相比,发现历时长达1小时的极端降雨强度普遍增加,而对于更长的历时,则既有增加也有减少。进行了子样本分析,以评估降雨数据中非平稳性的影响。区域模型将非平稳性作为不确定性的额外来源,连同抽样不确定性和由空间变异性引起的不确定性一起考虑。

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