首页|干旱区与湿润区旱涝急转演变特征对比研究

干旱区与湿润区旱涝急转演变特征对比研究

扫码查看
原文链接
  • 万方数据
  • 维普
以长江、黄河和淮河流域为研究对象，基于标准化旱涝急转指数，利用趋势分析、变点检验、小波分析、随机森林等方法探究典型干旱区与湿润区旱涝急转演变特征及其驱动因子。结果表明:湿润和半湿润区是极端旱涝急转事件的高频发生区，干旱区是极端旱转涝事件的高频发生区;干旱区的突变发生在1998年，湿润区的突变在1978年，未来干旱区更易发生旱转涝事件，湿润区则相反;气象因子在湿润区对旱涝急转的贡献度更大，大气环流对干旱区的影响突出，旱涝急转与不同驱动因子间存在非线性关系。
Comparative study on change characteristics of drought-flood abrupt alternation in arid and humid zones
Taking the Yangtze River,Yellow River,and Huai River basins as research objects,based on the standardized drought-wetness abrupt alternation index,this study explores the characteristics and driving factors of drought-flood abrupt alternation in typical arid and humid areas using methods such as trend analysis,change point test,wavelet analysis,and random forest.The results indicate that the humid/semi-humid areas are the high-frequency occurrence areas of extreme drought-flood abrupt alternation events,and the arid areas are the high-frequency occurrence areas of extreme drought to flood events.The mutation in arid areas occurred in 1998,while the mutation in humid areas occurred in 1978.In the future,arid areas are more prone to drought to flood events,while humid areas are the opposite.The contribution of meteorological factors to the rapid transition of drought and flood is greater in humid areas,and the impact of atmospheric circulation on arid areas is prominent.There is a non-linear relationship between the rapid transition of drought and flood and different driving factors.

drought-flood abrupt alternationstandardized drought-wetness abrupt alternation indexatmospheric circulationYangtze River BasinYellow River BasinHuai River Basin

薛联青、章郁涵、刘远洪

展开 >

河海大学水文水资源学院,江苏南京 210098

皖江工学院水利工程学院,安徽马鞍山 243031

旱涝急转 标准化旱涝急转指数 大气环流 长江流域 黄河流域 淮河流域

国家重点研发计划项目新疆生产建设兵团科技合作项目国家自然科学基金项目

2023YFC32068002022BC00151779074

2024

10.3880/j.issn.1004-6933.2024.04.001

水资源保护
河海大学 中国水利学会环境水利研究会

水资源保护

CSTPCD北大核心EI
影响因子：0.827
ISSN：1004-6933
年,卷(期)：2024.40(4)