For plots with surface residues, coefficient B is 0.41, and the constant C is 2.87. In the Mississippi River basin in northwestern Mississippi, Sharpe et al. These examples are listed in the table 2. 1.3318 4.3 A graph of these examples of the runoff calculation is shown in the following figure. Interception and bare soil water losses are calculated as fractions of the monthly precipitation and are subtracted from the total monthly precipitation, with the remainder of the water added to the soil.
Infiltration uses a bucket model to distribute water through the soil layers.
Water leached below the last soil layer is not available for evapotranspiration and is a measure of interflow, runoff or leaching losses from the soil profile. If erosion or deposition events occur, then recalculation will be done after the erosion and deposition is modelled. N, P, and S leaching respectively. The actual soil temperature used for decomposition and plant growth rate functions is the average of the minimum and maximum soil temperatures. This is a simple model of the temperature intertia in soils.