首页> 外文期刊>Fresenius environmental bulletin >STUDY ON THE DISTRIBUTION OF EXTREMEPRECIPITATION AND ITS POTENTIAL RISKS IN THEMIDDLE AND LOWER REACHES OFTHE YANGTZE RIVER IN CHINA
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STUDY ON THE DISTRIBUTION OF EXTREMEPRECIPITATION AND ITS POTENTIAL RISKS IN THEMIDDLE AND LOWER REACHES OFTHE YANGTZE RIVER IN CHINA

机译:中国长江中下游极度降水分布及其潜在风险的研究

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摘要

As global warming continues to intensify, ex- treme weather occurs from time to time, and extreme precipitation is the main cause of floods. For the middle and lower reaches of the Yangtze River in China, the analysis of extreme precipitation patterns is crucial to the prevention of flood risks. Regarding the extreme precipitation problem in the middle and lower reaches of the Yangtze River, in this paper, we have systematically analyzed the six indexes of ex- treme precipitation analysis in the middle and lowerreaches of the Yangtze River. Furthermore, two rela- tive precipitation indicators were proposed, namelytotal extreme precipitation (R99P) and total abnor- mal precipitation (R95P). According to the law of precipitation changes in the middle and lower reaches of the Yangtze River from 1960 to 2019, it is concluded that the highest value of the average an-nual precipitation is 1 348.92 mm from 1980 to 1989 On the whole, the average annual precipitation in the middle and lower reaches of the Yangtze River has a tendency to gradually decrease. The precipitation inthe middle and lower reaches of the Yangtze River is mainly concentrated in spring and summer. In the past 60 years, the precipitation intensity, maximum precipitation, number of consecutive days without precipitation, total extreme precipitation, and total abnormal precipitation in this area have all shown a gradual upward trend. This shows that extreme weather with rainfall in the middle and lower reachesof the Yangtze River is gradually increasing, and the risk of flooding will continue to increase.
机译:随着全球变暖的继续加剧,由于时间不时地发生,并且极端降水是洪水的主要原因。对于中国长江的中下游,对极端降水模式的分析对于预防洪水风险至关重要。在长江中下游的极端降水问题,在本文中,我们系统地分析了长江中下游的六个近辐射降水分析指标。此外,提出了两种重新定位的降水指示剂,NameelyToTal极端沉淀(R99P)和总Absor-Mal沉淀(R95P)。根据1960年至2019年的长江中下游降水变化规律,得出结论,平均沉淀的最高价值为1980年至1989年的平均值,平均值为148.92 mm长江中下游的年降水量逐渐减少。长江中下游的降水主要集中在春季和夏季。在过去的60年中,降水强度,最大降水,连续日期的次数连续,总极度降水和该区域的总异常降水都表现出逐渐上升趋势。这表明,长江中下游有降雨的极端天气逐渐增加,洪水的风险将继续增加。

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