Figure 3From: Impacts of climate change on regional hydrological regimes of the Wujiang River watershed in the Karst area, Southwest China Model components of the Karst distributed monthly hydrological model variable and parameters. Where η is the Pan evaporation conversion coefficient; 1–β1 is the proportion of fast flooding runoff in total runoff; β1×β2 is the proportion of the underground flow from small fractures in total runoff; WM is the average storage capacity; αF is the Fast flooding runoff; αM is the underground flow from large fractures and conduits; αS is the underground flow from small fractures) (Xue, 2010).Back to article page