IMHE OpenIR  > 山地灾害与地表过程重点实验室
Guo Xiaojun1; Cui Peng1; Li Yong1; Liu Jinfeng1; Ge Yonggang1; Wang Cide2
Source Publicationjournalofmountainscience
AbstractPeak discharge of flood in small mountainous watershed is usually calculated using the rainstorm-runoff calculation method in small watersheds in sichuan province (rrm). this study evaluated the rrm calculation using real-time monitored rainfall and hydrologic data from a small watershed in the wenchuan earthquake area of sichuan province, china. the results indicated that the discharge values given by the rrm are commonly overestimating the measured discharge. the overestimation rate was discussed and empirical equations were proposed for improving rrm estimations, based on the relationship between calculated and measured discharge values at different watershed scales (2, 30, and 40 km(2)), under different rainfall probabilities (0.97-0.5, 0.5-0.2, and 0.2-0.002), and for different rainfall durations (0-6, 6-24, and >24 h). the results of this study help contribute to the understanding of water floods formation and help provide more accurate estimations of peak flow discharge in small watersheds in the wenchuan earthquake area.
Document Type期刊论文
2.Aba Hydrological and Water Resources Survey Bureau of Sichuan Province
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
Guo Xiaojun,Cui Peng,Li Yong,et al. evaluationofatraditionalmethodforpeakflowdischargeestimationforfloodsinthewenchuanearthquakeareasichuanprovincechina[J]. journalofmountainscience,2019,16(3):641.
APA Guo Xiaojun,Cui Peng,Li Yong,Liu Jinfeng,Ge Yonggang,&Wang Cide.(2019).evaluationofatraditionalmethodforpeakflowdischargeestimationforfloodsinthewenchuanearthquakeareasichuanprovincechina.journalofmountainscience,16(3),641.
MLA Guo Xiaojun,et al."evaluationofatraditionalmethodforpeakflowdischargeestimationforfloodsinthewenchuanearthquakeareasichuanprovincechina".journalofmountainscience 16.3(2019):641.
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