1) T-hour unit hydrograph
时段单位线
1.
Traditional methods of deducing the T-hour unit hydrograph,such as the least-square method,are prone to create zigzagged oscillations of the resulting hydrographs,and the surface runoff depth is hardly equal to the net rainfall.
时段单位线被广泛应用于模拟流域中的地面径流过程。
3) instantaneous unit hydrograph
瞬时单位线
1.
Watershed instantaneous unit hydrograph based on information entropy theory;
基于信息熵理论的流域瞬时单位线
2.
Combining with a brief review of the basic conception on concentration curves of flood waves in river and instantaneous unit hydrograph in watershed,the unit(or dimension) of some common-used concentration curves are analyzed,interpreted in detail and given clearly.
结合河段洪水演算法及流域汇流瞬时单位线法中几种汇流曲线的基本概念,对汇流曲线的单位(因次)问题进行了分析和解释,明确给出了汇流曲线的单位(因次)。
5) lag-instantaneous unit hydrograph
迟滞瞬时单位线
1.
Parameter estimation for lag-instantaneous unit hydrograph with entropy method;
迟滞瞬时单位线参数估计熵法
6) watershed geomorphology instantaneous unit hydrograph
流域瞬时单位线
补充资料:比例线段
[编辑] 比例线段
[解释]
在同一单位下,四条线段长度为a、b、c、d,其关系为a:b=c:d,那么,这四条线段叫做成比例线段或简称比例线段。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条