Certain Flood-Flow Phenomena of Iowa Rivers

Nagler, Floyd A.

doi:10.1175/1520-0493(1933)61<5:cfpoir>2.0.co;2

Mon. Wea. Rev.

1933

DOI: 10.1175/1520-0493(1933)61<5:cfpoir>2.0.co;2

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Certain Flood-Flow Phenomena of Iowa Rivers

Floyd A. Nagler¹

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“…Probably these rains were con centrated in small areas lying between the reporting stations. The characteristic double peak in Iowa City which ordinarily results from a single rainstorm has been discussed by the late Pro fessor F. A. Nagler [6].…”

mentioning

confidence: 99%

The structure of discharge‐recession curves

Barnes¹

1939

Eos Trans. AGU

242

156

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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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mentioning

confidence: 99%

The structure of discharge‐recession curves

Barnes¹

1939

Eos Trans. AGU

242

156

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100 Years of Progress in Hydrology

Peters‐Lidard

Hossain

Leung

et al. 2018

Meteorological Monographs

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Certain Flood-Flow Phenomena of Iowa Rivers

Cited by 2 publications

References 0 publications

The structure of discharge‐recession curves

The structure of discharge‐recession curves

100 Years of Progress in Hydrology

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