The rising and recession limbs of conceptual dimensionless overland fl
ow hydrographs are calculated for specific values of the rating expone
nt in the range 1 less than or equal to m less than or equal to 3, inc
luding a linear reservoir (m = 1): 100% turbulent Chezy friction (m =
3/2); 100% turbulent Manning friction (m = 5/3): 67% turbulent Chezy (
or 75% turbulent Manning) (m = 2); and 100% laminar flow (in = 3). The
se conceptual overland Bow hydrographs show finite amounts of diffusio
n, increasing with decreasing rating exponent, unlike the kinematic wa
ve hydrograph, which is nondiffusive. (C) 1997 Elsevier Science B.V.