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VIC模型在柯街河流域降雨量—流量模拟过程中的应用

Application of VIC(Variable Infiltration Capacity) Model to Rainfall-Runoff Simulation in the Reach of Kejie River
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摘要 采用0.01°×0.01°为基本计算单位,以1999年1月至2000年12月为模拟时段。应用水文变量渗透模型反复推算,结果显示,水文站观测流量曲线基本与模型计算出的流量曲线一致。尽管存在数据可供性和模拟精确度的限制,水文变量渗透模型仍然可以预测流域水文变化和全球气候变化趋势。 0. 01 × 0. 01 resolution (about 0. 6 km?) as basic unit is adopted, and simulative period is from Jan of 1999 to Dec of 2000. The repetitive calculation by VIC model indicates that runoff curve observed is almost same as that calculated. Although there exit some limits on the data accessibility and simulative precision, VIC model still can predict the global climate change and watershed hydrological change.
出处 《林业调查规划》 2006年第5期118-121,共4页 Forest Inventory and Planning
关键词 水文变量渗透能力模型(VIC模型) 降雨量 流量 模拟过程 柯街河流域 Variable Infiltration Capacity (VIC model) rainfall runoff simulation in the reach of Kejie River
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