Upstream boundary conditions are required at the upstream end of all reaches that are not connected to other reaches or storage areas. An upstream boundary condition is applied as a flow hydrograph of discharge versus time. The equation of a flow hydrograph for reach m is:

1) \displaystyle \Delta Q_k^{n+1} = Q_k^n - Q_k

where k is the upstream node of reach m. The finite difference form of (1) is:

2) MUQ_m \Delta dQ_K = MUB_m
SymbolDescription

MUQ_m

1

MUB_m

Q_1^{n+1} - Q_1^n

Typical flow split and combination.