## Abstract This paper deals with the derivation of the hydrological response of a hillslope on the assumption of quick runoff by surface runoff generation. By using the simple nonβlinear storage based model, first proposed by Horton, an analytical solution of the overland flow equations over a pla
A simple overland flow calculation method for distributed groundwater recharge models
β Scribed by M. M. Mansour; A. Barkwith; A. G. Hughes
- Publisher
- John Wiley and Sons
- Year
- 2011
- Tongue
- English
- Weight
- 896 KB
- Volume
- 25
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.8074
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π SIMILAR VOLUMES
In simulating two-phase flows, interface normal vectors and curvatures are needed for modeling surface tension. In the traditional approach, these quantities are calculated from the spatial derivatives of a scalar function (e.g. the volume-offluid or the level set function) at any instant in time. T
The nonlinearly coupled Vlasov-Maxwell ion-plasma field equations are solved exactly for a transversely uniform subgroup of rotational modes induced by a uniform axial magnetic field. The ion orbits in momentum space are bipolar doubly periodic eigenfunctions of ion proper time, obtained in closed f