1) storage capacity of watershed
汇水流域蓄水量
2) storage capacity of watershed
汇水流域内的蓄水量
3) river basin water storage
流域蓄水量
1.
Thus,the model was improved in two aspects: a new formula for calculation of evaportranspiration was constructed with the effects of precipitation and river basin water storage at former stage on evapor.
结果表明,较之原模型,改进后的模型精度更高,月径流计算过程与实测过程拟合效果较好,年内最大洪峰流量相对误差明显减小,模拟的月蒸散发和流域蓄水量过程更加合理。
4) Upslope runoff rate
汇水流量
5) watershed storage capacity curve
流域蓄水容量曲线
1.
Only the influence of spatial heterogeneity of underlying surface factors on watershed runoff yield under the situation of the spatial homogeneity of rainfall can be considered with the method of watershed storage capacity curve and infiltration capacity area distribution curve.
流域蓄水容量曲线和下渗能力面积分配曲线只能考虑降雨空间分布均匀时下垫面因子空间分布不均匀对流域产流量的影响。
6) rainwater catchments basin
雨水流域汇水区
1.
Automatic partition of urban rainwater catchments basin;
城市雨水流域汇水区自动划分
补充资料：内流流域
又称“内流区”。指地表径流不能流注海洋的地区，即内流河流域范围。一般分布在远离海洋或为山脉环抱的内陆地区。气候干燥，蒸发强烈，河道稀疏，水量贫乏，河流多注入内陆湖泊或中途消失。
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