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Section 2: Hydrology

The land phase of the hydrologic cycle is based on the water balance equation:

SWt=SW0+∑i=1t(Rday−Qsurf−Ea−wseep−Qgw)SW_t = SW_0 +\sum_{i=1}^t (R_{day} - Q_{surf} - E_a - w_{seep} - Q_{gw})SWt​=SW0​+i=1∑t​(Rday​−Qsurf​−Ea​−wseep​−Qgw​)

where SWtSW_tSWt​ is the final soil water content (mm H2O), SW0SW_0SW0​ is the initial soil water content (mm H2O), t is the time (days), RdayR_{day}Rday​ is the amount of precipitation on day i (mm H2O), QsurfQ_{surf}Qsurf​ is the amount of surface runoff on day i (mm H2O), EaE_aEa​ is the amount of evapotranspiration on day i (mm H2O), wseepw_{seep}wseep​ is the amount of percolation and bypass flow exiting the soil profile bottom on day i (mm H2O), and QgwQ_{gw}Qgw​ is the amount of return flow on day i (mm H2O).