The consistency of the calculated groundwater level and the measured shows this simulation model can well reflect the actual hydrogeological condition. 結果表明，計算模型與實(shí)際水文地質(zhì)條件比較接近，計算水位與實(shí)測水位相吻合。
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. 進(jìn)一步的工作是要把這樣的地下徑流模型與地下水位動(dòng)態(tài)表示的土壤水模型應用于氣候模擬。
