The most extreme rainfall erosivity event ever recorded in China up to 2022: the 7.20 storm in Henan Province

IF 5.7 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Yuanyuan Xiao, S. Yin, Bofu Yu, Conghui Fan, Wenting Wang, Yun Xie
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Abstract

Abstract. Severe water erosion occurs during extreme storm events. Such an exceedingly severe storm occurred in Zhengzhou in central China on 20 July 2021 (the 7.20 storm). The magnitude and frequency of occurrence of this storm event were examined in terms of how erosive it was. To contextualize this extreme event, hourly rainfall data from 2420 automatic meteorological stations in China from 1951 to 2021 were analyzed to (1) characterize the spatial and temporal distribution of the rainfall amount and rainfall erosivity of the 7.20 storm, (2) evaluate the average recurrence interval of the maximum daily and event rainfall erosivity, and (3) establish the geographical distribution of the maximum daily and event rainfall erosivity in China. The center of the 7.20 storm moved from southeast to northwest in Henan Province, and the most intense period of rainfall occurred in the middle and late stages of the storm. Zhengzhou Meteorological Station happened to be aligned with the center of the storm, with a maximum daily rainfall of 552.5 mm and a maximum hourly rainfall intensity of 201.9 mm h−1. The average recurrence intervals of the maximum daily rainfall erosivity (43 354±1863 MJ mm ha−1 h−1) and the maximum event rainfall erosivity (58 874±2351 MJ mm ha−1 h−1) were estimated to be about 19 200 and 53 700 years, respectively, assuming the log-Pearson type-III distribution, and these were the maximum rainfall erosivities ever recorded among 2420 meteorological stations in mainland China up to 2022. The 7.20 storm suggests that the most erosive of storms does not necessarily occur in the wettest places in southern China, and these can occur in mid-latitude around 35∘ N with a moderate mean annual rainfall of 566.7 mm in Zhengzhou.
截至 2022 年中国有记录的最极端降雨侵蚀事件:河南省 7.20 特大暴雨
摘要在极端暴雨事件中会发生严重的水土流失。2021 年 7 月 20 日,中国中部郑州发生了一次特大暴雨(7.20 暴雨)。我们从侵蚀程度的角度研究了这次暴雨事件的规模和发生频率。为了解这一极端事件的来龙去脉,我们分析了 1951 年至 2021 年中国 2420 个自动气象站的小时降雨量数据,以便:(1) 描述 7.20 暴雨的降雨量和降雨侵蚀率的时空分布特征;(2) 评估最大日降雨侵蚀率和事件降雨侵蚀率的平均重现间隔;(3) 确定中国最大日降雨侵蚀率和事件降雨侵蚀率的地理分布。7.20 风暴中心在河南省由东南向西北移动,最强降雨时段出现在风暴的中后期。郑州气象站恰好与暴雨中心重合,最大日降雨量为 552.5 毫米,最大小时降雨量为 201.9 毫米/小时-1。假设对数-皮尔逊Ⅲ型分布,最大日降雨侵蚀率(43 354±1863 MJ mm ha-1 h-1)和最大事件降雨侵蚀率(58 874±2351 MJ mm ha-1 h-1)的平均重现间隔分别约为 19 200 年和 53 700 年,是截至 2022 年中国大陆 2420 个气象站记录到的最大降雨侵蚀率。7.20暴雨表明,侵蚀性最强的暴雨并不一定发生在中国南方最潮湿的地方,这些暴雨可能发生在北纬35∘左右的中纬度地区,郑州的年平均降雨量为566.7毫米,属于中等水平。
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来源期刊
Hydrology and Earth System Sciences
Hydrology and Earth System Sciences 地学-地球科学综合
CiteScore
10.10
自引率
7.90%
发文量
273
审稿时长
15 months
期刊介绍: Hydrology and Earth System Sciences (HESS) is a not-for-profit international two-stage open-access journal for the publication of original research in hydrology. HESS encourages and supports fundamental and applied research that advances the understanding of hydrological systems, their role in providing water for ecosystems and society, and the role of the water cycle in the functioning of the Earth system. A multi-disciplinary approach is encouraged that broadens the hydrological perspective and the advancement of hydrological science through integration with other cognate sciences and cross-fertilization across disciplinary boundaries.
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