This document describes how to derive a required time (T) unit hydrograph from a given time (D) unit hydrograph when T is not a multiple of D using the S-curve method. It explains that an S-curve hydrograph is generated by continuous, uniform effective rainfall and rises continuously in the shape of an S until equilibrium is reached. The ordinates of the S-curve can be calculated using the equation S(t) = U(t) + S(t-D), where S(t) is the ordinate of the S-curve at time t, U(t) is the ordinate of the given unit hydrograph at time t, and S(t-D) is the