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- W2006157035 abstract "In their comment, Cao and Yue (2006) present a criticism of the momentum source term due to infiltration presented in Mudd (2006). Cao and Yue (2006) argue that because water infiltrating into the bed of a channel during a flash flood has no downstream component of velocity, the momentum sink term due to infiltration described in Mudd (2006) should be equal to zero. In addition, they argue that because rainfall has no downstream velocity component, it too has no effect on momentum, and the source terms that appear in ElHames and Richards (1998) are also incorrect. Because there are inconsistencies in the terms used in the momentum equations for infiltration and rainfall (e.g., Bras, 1990; Cunge et al., 1980; El-Hames and Richards, 1998; Mudd, 2006), here I address the comments of Cao and Yue (2006) and clarify the role of rainfall at the surface and infil-" @default.
- W2006157035 created "2016-06-24" @default.
- W2006157035 creator A5044968443 @default.
- W2006157035 date "2007-03-01" @default.
- W2006157035 modified "2023-09-25" @default.
- W2006157035 title "Reply to “Comment on ‘Investigation of the hydrodynamics of flash floods in ephemeral channels: Scaling analysis and simulation using a shock-capturing flow model incorporating the effects of transmission losses’ by S.M. Mudd, 2006 (Journal of Hydrology) 324, 65–79” by Cao and Yue" @default.
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- W2006157035 doi "https://doi.org/10.1016/j.jhydrol.2006.11.008" @default.
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