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USGS · 70221653

Bank storage‐loss and recovery of Missouri River discharge during drought of 1934

H.C. Beckman
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Abstract

Whenever measurements show that the discharge of a stream becomes smaller as it passes downstream to a considerably larger drainage-area and no diversions of water are known to exist between the places of measurement, curiosity is always aroused as to the cause, and a question may be raised as to the accuracy of the measurements purporting to show the decrease. Small streams sometimes disappear in fault-planes and crevices in rocky regions with relatively high slopes, or in flat sand- and gravel-bars, and then reappear full-size farther downstream. This behavior, however, represents no decrease in the discharge but merely means that the stream is following an underground rather than a surface-course for that part of its travel.

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BibTeXRIS

H.C. Beckman. 2014-08-18. Bank storage‐loss and recovery of Missouri River discharge during drought of 1934. https://doi.org/10.1029/tr016i002p00513

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