| 1. | An research on underground runoff deciding flood forecast model
以地下径流为主的洪水预报模型研究 |
| 2. | A study on the structure of karst aquifer medium and the groundwater flow in houzhai underground river basin
后寨河流域岩溶含水介质结构与地下径流研究 |
| 3. | Furthermore , soil and water conservation also resulted in the underground flow decrease but its decrease extent is smaller than of surface flow
水土保持也使河川地下径流量有所减少，但降低程度较地表径流量小。 |
| 4. | The next work is to apply this subsurface runoff model and the soil moisture model with dynamic representation of the groundwater table to climate simulations
进一步的工作是要把这样的地下径流模型与地下水位动态表示的土壤水模型应用于气候模拟 |
| 5. | The modeled base - flow values are compared to the results from a simple base flow separation algorithm . in this study , we use the one - parameter algorithm described by chapman 33
采用chapman所提出的单参数地下径流分离算法33从观测的径流资料中分离出地下径流量 |
| 6. | In this paper , a physics - based subsurface runoff parameterization with water storage and recharge based on the boussi - nesq - storage equation is presented . this paper is or - ganized as follows
1基于boussinesq - storage方程的地下径流机制下面主要是以潜水面上的boussinesq方程为基础来建立地下径流模型 |
| 7. | Therefore , the development of the surface runoff and subsurface run - off mechanisms , and a soil moisture model that can represent the hydrological processes correctly is sig - nificant in improving land surface modeling
因此,发展合适的地表地下径流机制以及土壤水模型对于改进陆面水文模拟具有重要的的意义 |
| 8. | Now , the b - s subsurface runoff model and the soil moisture model with with dynamical representation of the groundwater table have both been coupled to the community land model 25 , 30 to perform some validation simulations
其次将该地下径流机制与地下水位动态表示的土壤水模型一起耦合到陆面模式clm 25 , 26里作验证试验 |
| 9. | One exception is tu - wei - he catchment where underground runoff is the primary part of river flow . its runoff season distribution is much uniformity . its runoff amount of july to august accounts is 24 % of the annual runoff amount
但以地下径流补给为主的秃尾河，径流量的季节分配相对均匀， 7 8月份径流量占年径流量的24 。 |
| 10. | Change of surface runoff and land subsurface runoff would result in change of soil moisture and water and energy bal - ance between the land surface and atmosphere and would ultimately influence climate
地表地下径流的改变都会引起土壤水分含量的变化,进一步影响到陆地表面与大气之间的水分通量与热通量的变化,从而对气候产生影响 |
