Hydrological component of the Achelous model

The runoff from an area can be expressed in the following water balance equation:

R = P – ΔS – ΔM – E

where R = runoff

P = precipitation in the form of rain

ΔS = change in storage due to snow cover

ΔM = other change in storage (ground, lakes and groundwater)

E = evaporation

These parameters are calculated with the aid of several sub-models described below.