摘要
针对小流域降雨资料不足甚至无降雨资料的情况,研究了在不同雨型(主雨位偏前、偏中和偏后)下,使用2种暴雨频率计算方法(地区综合法和L-矩法),计算不同重现期设计暴雨和设计洪水的不确定性。结果表明L-矩法的计算结果不确定性小,更稳定,而地区综合法偏保守;不同雨型下的设计洪峰和洪水历时变化较小,但峰现时间相差较大,会极大地影响调洪结果。
Estimating design flood in ungauged catchments is difficult due to data scarcity. Two methods, regional synthetic method and L-moment, are used to calculate design rainfall depths, and thus to estimate design flood. Also, three different 24-hour-hyetographs are considered, with front-, mid-, back- located peak rainfall. A small ungauged catchment in Zhejiang Province is used as an example here and results show that the regional synthetic method is more conservative than L-moment and contains more uncertainty. Delicate peak change discharge for different hyetographs can be observed while peak times are different, which is believed to affect reservoir routing significantly.
出处
《中山大学学报(自然科学版)》
CAS
CSCD
北大核心
2008年第6期61-65,69,共6页
Acta Scientiarum Naturalium Universitatis Sunyatseni
基金
浙江省自然科学基金资助项目(Y507071)
浙江省水利厅项目(N20070066)