Saturation Excess Flow
Saturation Excess Flow is a type of hydrological runoff process in which surface water accumulation occurs when precipitation or meltwater input exceeds the capacity of the soil profile to transmit water, causing the water table to rise to the surface and generate flow over saturated areas, distinguished from infiltration-excess overland flow by its dependence on subsurface saturation dynamics rather than surface infiltration limits.
84
Publications
6.3K
Citations
255
Authors
122
Institutions
Publications per year
2017–2026
8
Variants
Dunne Overland FlowDunne Runoff
Parents
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1–5 of 84
255
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University of Illinois Urbana-Champaign, United States
6 publications · 631 citations
6
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5
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4
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1–5 of 255
122

Cornell University
Ithaca, United States
15 h-index
54 publications
3.6K citations

Bahir Dar University
Bahir Dar, Ethiopia
8 h-index
22 publications
1.1K citations
Virginia Tech
Blacksburg, United States
5 h-index
7 publications
393 citations
Amhara Agricultural Research Institute
Bahir Dar, Ethiopia
4 h-index
5 publications
195 citations
University of South Florida
Tampa, United States
4 h-index
10 publications
204 citations

The University of Western Australia
Perth, Australia
4 h-index
6 publications
260 citations
Princeton University
Princeton, United States
4 h-index
5 publications
170 citations
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering
Nanjing, China
3 h-index
11 publications
241 citations
1–8 of 122
17 publications · 1.2K citations
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11 publications · 2.5K citations
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11 publications · 1K citations
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6 publications · 353 citations
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5 publications · 170 citations
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