1. China Institute of Water Resources and Hydropower Research, Beijing 100038; 2. Research Center on Flood and Drought Disaster Reduction of the Ministry of Water Resources, Beijing 100038; 3. College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002
Abstract:As a typical humid-semi humid area,the temporal and spatial distribution characteristics of drought disasters in the Yangtze River basin are complicated.In order to analyze the risk distribution characteristics of drought disasters in the Yangtze River basin,based on the multi-source statistical data of drought disasters from 1990 to 2020,the method of drought disaster risk assessment was used to analyze agricultural drought,drinking water difficulty and comprehensive risks.The results show that the spatial distribution of agricultural drought disaster risk in different regions of the Yangtze River basin is quite different,and the risk level of some districts and counties in Sichuan,Hunan,Hubei,Jiangxi and Yunnan provinces is on the high side;High/medium high risk areas of drinking water difficulty due to drought are mainly concentrated in Guizhou,Hubei,Hunan,Sichuan provinces and Chongqing City,and mainly distributed in mountainous areas with weak water facilities;The spatial distribution of drought disaster comprehensive risk shows that the general risk level of traditional arid areas such as Sichuan basin,central Yunnan plateau,central Guizhou,Heng Shao Drought corridor,Jitai basin,northern Hubei hillock,central Hubei hilly area,and southern Hunan is high,which is consistent with the severe drought area of the Yangtze River basin in 2022.
陈茜茜, 屈艳萍, 吕娟, 常文娟. 长江流域干旱灾害风险分布特征分析[J]. 中国防汛抗旱, 2022, 32(10): 17-22.
CHEN Xixi, QU Yanping, LYU Juan, CHANG Wenjuan. Study on the spatial and temporal distribution characteristics of drought disasters in the Yangtze River basin. journal1, 2022, 32(10): 17-22.
[1] DAI A G. Increasing drought under global warming in observations and models[J]. Nature Climate Change, 2013, 3(1):52-58. [2] SU B D, HUANG J L, FISCHER T, et al. Drought losses in China might double between the 1.5℃ and 2.0℃ warming[J]. Proceedings of the National Academy of Sciences of the United States of America, 2018, 115(42):10600-10605. [3] 屈艳萍,吕娟,苏志诚,等.抗旱减灾研究综述及展望[J].水利学报, 2018, 49(1):115-125. [4] 屈艳萍,吕娟,程晓陶,等.干旱相关概念辨析[J].中国水利水电科学研究院学报, 2016, 14(4):241-247. [5] 张学君,吕娟,屈艳萍,等.湄公河流域气象和水文干旱时空演变特征与规律分析[J].河北水利电力学院学报, 2021, 31(2):1-6, 16. [6] 黄涛,徐力刚,范宏翔,等.长江流域干旱时空变化特征及演变趋势[J].环境科学研究, 2018, 31(10):1677-1684. [7] 梁成,申双和.基于WAP指数的长江流域及其以南地区干旱气候特征分析[J].南京信息工程大学学报(自然科学版), 2010, 2(2):166-174. [8] 刘君龙,袁喆,许继军,等.长江流域气象干旱演变特征及未来变化趋势预估[J].长江科学院院报, 2020, 37(10):28-36. [9] 许继军,杨大文,雷志栋,等.长江流域降水量和径流量长期变化趋势检验[J].人民长江, 2006(9):63-67.