摘要
针对坡面径流模拟算法引入集水面积阈值划分流域内的河网与坡地直接影响了生成的数字河网精度,探讨并比较了多种推求流域集水面积阈值的方法。结果表明,各种方法可互补;采用集水面积与河道平均坡降关系和采用集水面积与河网密度曲线具有较好的一致性;流域面积越大,采用宽度分布推求阈值准确,流域面积越小,采用水系分形推求阈值准确;集水面积阈值在流域内各处并非完全相同,应考虑采用多个阈值。
The critical support area, as a vital parameter in the method, defines the minimum drainage area required to divide hillslopes and channels and ultimately has its impact on the precision of extracted drainage network. Four methods for identifying critical support area are discussed and compared in this paper, including the relation between contributing area and topographic slope, the drainage network density method, the width function method and the fractal method. The computed results show that the above ways of identifying critical support area can be complementary. The result from the relation between contributing area and topographic slope is in good agreement with that computed by the method of drainage network density. The river width function method is more suitable in larger catchment while the fractal method is appropriate in small watershed. Thus it is recognized that different values of critical support areas should be specified within a large scale of catchment because of spatial variability.
出处
《水电能源科学》
北大核心
2009年第5期11-14,171,共5页
Water Resources and Power
基金
国家863计划课题基金资助项目(2008AA12Z202)
水利公益性行业科研专项基金资助项目(2007SHZ1-1)
教育部和国家外专局"111计划"基金资助项目(B08048)
关键词
集水面积阈值
数字高程模型
数字水系
分形
河网宽度
critical support area
digital elevation model
digital drainage network
fractal
river width function