文摘
Incorporated dynamic ecohydrological processes into Budyko–Choudhury–Porporato (BCP) model. Above, linked to typical soil water ‘bucket’ model, results in the dynamic BCP (dBCP) model. dBCP allows Choudhury’s n-value to be calculated dynamically. Assessed actual evapotranspiration (E) changes for different vegetation cover fractions. Analytically assessed the sensitivity of E to changes in P, Ep, effective rooting depth and storm depth.