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Regional Variability of Mean Annual Water Balance for Non-humid Catchments in Northern China Based on the Budyko Hypothesis

机译:基于Budyko假设的中国非湿度集水区的平均水平的区域变异性

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Based on long-term mean of climate and discharge in 108 non-humid catchments in Northern China, this study analyzed the regional variability of mean annual water balance based on the Budyko hypothesis. Besides the annual climate conditions, the regional pattern of water-energy balance is also correlated to the relative infiltration capacity (K_s/i_r), relative soil water storage (S_(max)/E_0), and the average slope (tanβ). This study proposed an empirical formula to enable one to estimate the parameter ω in Fu's equation (1981) from catchment characteristics without calibration from the long-term water balance. It has been shown that Fu's equation together with the parameter at estimated by this empirical formula can predict accurately the mean annual evapotranspiration.
机译:基于中国北方108个非湿度集水区的长期依据,本研究分析了基于Budyko假设的平均水平的区域变异性。 除了年度气候条件外,水能平衡区域模式也与相对渗透能力(K_S / I_R),相对土壤储水(S_(MAX)/ E_0)和平均斜坡(TANβ)相关。 本研究提出了一种经验公式,使得能够从集水区估计FU的等式(1981)中的参数ω,而不会从长期水平衡校准。 已经证明,傅氏等式与该经验公式估计的参数一起可以准确地预测平均年度蒸散。

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