Infiltration Excess Flow

Infiltration Excess Flow is a type of surface and subsurface hydrological flow process wherein water moves downslope along soil-bedrock interfaces due to the saturation of infiltration capacity, distinguished from other flow types by its dependence on precipitation intensity exceeding soil infiltrability.

74

Publications

3.9K

Citations

257

Authors

141

Institutions

Publications per year

2017–2026

10

Variants

Horton Overland Flow

Authors

257

  1. MS
    Murugesu Sivapalan

    University of Illinois Urbana-Champaign, United States

    7 publications · 664 citations

    7

    h-index

  2. TS
    Tammo S. Steenhuis

    Cornell University, United States

    6 publications · 449 citations

    6

    h-index

  3. KB
    Keith Beven

    Lancaster University, United Kingdom

    4 publications · 760 citations

    4

    h-index

  4. AS
    Amy S. Collick

    Cornell University, United States

    3 publications · 278 citations

    3

    h-index

  5. EF
    Eric F. Wood

    Princeton University, United States

    3 publications · 538 citations

    3

    h-index

1–5 of 257

Venues

  1. Hydrological Processes

    21 publications · 1.3K citations

    18

    h-index

  2. Water Resources Research

    10 publications · 1K citations

    10

    h-index

  3. Journal of Hydrologic Engineering

    6 publications · 157 citations

    6

    h-index

  4. Hydrological Sciences Journal

    3 publications · 108 citations

    3

    h-index

  5. Journal of Hydrology and Hydromechanics

    2 publications · 38 citations

    2

    h-index

1–5