Different responses of event-based flood to typhoon and non-typhoon rainstorms under land use change in Xixi Basin of southeastern China

被引:1
|
作者
Cheng, Hong [1 ]
Lin, Bingqing [4 ]
Ying, Siran [1 ]
Chen, Xingwei [1 ,2 ,3 ]
Chen, Qingyong [5 ]
Yao, Huaxia [6 ]
机构
[1] Fujian Normal Univ, Coll Geog Sci, Fuzhou 350007, Peoples R China
[2] Fujian Engn Res Ctr Land Disaster Monitoring & Ass, Fuzhou 350007, Peoples R China
[3] State Key Lab Breeding Base Humid Subtrop Mt Ecol, Fuzhou 350007, Peoples R China
[4] Quanzhou Normal Univ, Coll Resources & Environm Sci, Quanzhou 362000, Peoples R China
[5] Fujian Hydrol & Water Resources Survey Ctr, Fuzhou 350007, Peoples R China
[6] Minist Environm Conservat & Pk, Inland Waters Unit, Dorset, ON P0A 1E0, Canada
关键词
Flood; Typhoon; Land use change; Frequency analysis; HEC-HMS model; HYDROLOGIC MODELING SYSTEM; TROPICAL CYCLONES; RAINFALL VARIABILITY; DISTRIBUTIONS; IMPACTS; RUNOFF; TRENDS; RIVER;
D O I
10.1016/j.catena.2023.107562
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
There are two major types of rainstorms in the Asia-Pacific region -typhoon induced rainstorm and non-typhoon rainstorm. This study investigated and separated the different flood responses to these two types of rainstorms, based on a scheme that combined the classification of typhoon and non-typhoon rainstorm floods, the simulation from a distributed hydrological model, and a method to forward restore the impact of land use change on flood frequency analysis. For flood events in a typical basin on the southeast coast of China, the flood characteristics in response to typhoon and non-typhoon rainstorms were significantly different in three aspects: (1) The key parameters in the HEC-HMS model were systematically different. The initial loss and wave velocity of the model were apparently larger for the typhoon rainstorm flood than for the non-typhoon rainstorm flood. (2) The impacts of land use change were different, with smaller effect on typhoon induced floods than on non-typhoon floods under the same magnitude of flood peak flow. (3) Classification of two types of floods resulted in more reasonable frequency analysis affected with the land use change because the annual maximum flood series is the mixture of typhoon and non-typhoon rainstorms. Frequency analysis for the forward-restored mixture flood series showed that the land use change with the decrease in the area of forest land and the increase of garden and construction land resulted in the increase of the mean maximum flow from 2266.6 to 2510.19 m3/s, but the values of coefficient of variation were slightly altered, the ratio of skewness coefficient to variation coefficient were unchanged. The results provide new ideas and methods for a deeper understanding of the impact of land use change on flooding in typhoon and non-typhoon co-action regions.
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页数:11
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