The concept of ‘reverse’ flow routing in rivers is proposed, in which upstream flow hydrographs are specified from a downstream flow requirement. An example is given of reverse flow routing by the implicit method of solution of the equations of momentum and continuity. Reverse flow routing is further described in the context of the x-t plane, and then the point is made that solutions were not
... [Show full abstract] found in all possible directions of computation in the x-t plane. Solutions were found only in the directions of increasing time and decreasing distance (upstream).