Discussion of “Cochrane on Rainfall Intensities and Frequencies”

Storm‐discharge of streams in the upper Mississippi Valley consists of surface‐flow and storm‐seepage. The total runoff, resulting from a storm, of either of these components does not bear a fixed relation to the runoff of the other. The two are influenced by different sets of conditions. The two components of the storm‐flow can be separated by graphical analysis. A reversal of the process has been found useful in determining the hydrograph of ground‐water flow.

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The structure of discharge‐recession curves

Barnes¹

1939

Eos Trans. AGU

243

156

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Discussion of “Cochrane on Rainfall Intensities and Frequencies”

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The structure of discharge‐recession curves

The structure of discharge‐recession curves

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