The National Weather Service 1D dynamic flood routing model FLDWAV is enhan
ced to include capability of modeling mud/debris unsteady flows by includin
g an additional friction slope term in the momentum equation of the Saint-V
enant equations. Three techniques are incorporated into the model to determ
ine the mud/debris related friction slope term due to the internal viscous
dissipation of non-Newtonian fluids and granular sliding friction of coarse
-grained debris surges. These techniques are tested and some computational
results are compared with observed field data and experimental data.