区域地下水资源利用潜力与水文循环陆地过程相关。
The latent capacity of utilizing groundwater is variable, which depends on the land processes of the regional hydrologic cycle.
试验表明陆地水储量月变化在水文模型中主要反映为土壤水分的变化，与前人的研究结果吻合。
The results show that changes in total water storage on hydrological model reflects the changes mainly as soil moisture change, which is consistent with the previous.
与水文模型比较的验证性实验结果，也证明了GRACE数据估算的水储量变化是陆地水储量变化的总量。
Compared with the hydrological model data, the result also proved the GRACE based water storage estimating the total terrestrial water storage.
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