Natural stream channel‐storage (second paper)
- 1 July 1937
- journal article
- Published by American Geophysical Union (AGU) in EOS, Transactions American Geophysical Union
- Vol. 18 (2) , 440-456
- https://doi.org/10.1029/tr018i002p00440
Abstract
Introduction‐Synopsis—The runoff‐rate and runoff‐graph at an outlet or point on the stream‐channel are not the same as the rate and graph of direct surface‐runoff from the area upstream from the outlet, owing to the fact that the direct surface‐runoff is modified by channel‐storage.The author's first paper on this subject (Trans. Amer. Geophys. Union, 1936, pp. 408–415) gives a method of determining the volume of stream channel‐storage during recession of a stream‐rise. It is shown that the volume and outflow‐rates from channel‐storage, exclusive of groundwater, are related through the equations.Keywords
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