Construct · 1 fields · 1 citations

saturation-excess overland flow: a standalone construct

One name. One construct. A landmark on the map.

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saturation-excessoverland flow1 CONSTRUCTSaturation-excessDUNNE · HYDROLOGY

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Hydrology

surface runoff that occurs when the soil becomes saturated from below so further rain cannot infiltrate, typically near streams.

In hydrology, saturation-excess overland flow refers to surface runoff that occurs when the soil becomes saturated from below so further rain cannot infiltrate, typically near streams. This meaning comes from Dunne (1970) in Water Resources Research.[1]

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Nearby constructs

flow6 names · 12 citationsjangle · five names, one experience, partlyrunoff2 fields · 4 citationsjingle · one word, two constructssurface3 fields · 3 citationsjingle · one word, three constructs

References

  1. Dunne, T., & Black, R. D. (1970). Partial Area Contributions to Storm Runoff in a Small New England Watershed. Water Resources Research, 6(5), 1296-1311. https://doi.org/10.1029/wr006i005p01296

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