The Muskingum model of routing a flood through a stream reach is expressed as O2=K0I2+K1I1+K2O1 where K0, K1, and K2 are routing coefficient for the concerned reach; I1 and I2 are the inflows to the reach and O1 and O2 are the outflows from the reach corresponding to time steps 1 and 2 respectively. The sum of K0, K1 and K2 of the model is