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

Authors

255

  1. TS
    Tammo S. Steenhuis

    Cornell University, United States

    15 publications · 863 citations

    13

    h-index

  2. ZM
    Zachary M. Easton

    Virginia Tech, United States

    7 publications · 392 citations

    7

    h-index

  3. MS
    Murugesu Sivapalan

    University of Illinois Urbana-Champaign, United States

    6 publications · 631 citations

    6

    h-index

  4. SA
    Seifu A. Tilahun

    Bahir Dar University, Ethiopia

    5 publications · 173 citations

    5

    h-index

  5. BY
    Birru Yitaferu

    Amhara Agricultural Research Institute, Ethiopia

    4 publications · 135 citations

    4

    h-index

1–5 of 255

Venues

  1. Hydrological Processes

    17 publications · 1.2K citations

    16

    h-index

  2. Water Resources Research

    11 publications · 2.5K citations

    11

    h-index

  3. Hydrology and earth system sciences

    11 publications · 1K citations

    11

    h-index

  4. Journal of Hydrologic Engineering

    6 publications · 353 citations

    6

    h-index

  5. Hydrological Sciences Journal

    5 publications · 170 citations

    5

    h-index

1–5