Hortonian Runoff

Hortonian Runoff is a type of surface runoff process in hydrology whereby overland flow is generated when rainfall intensity exceeds the infiltration capacity of the soil, leading to the accumulation and downslope movement of water on the land surface.

56

Publications

3.3K

Citations

153

Authors

91

Institutions

Publications per year

2017–2026

6

Variants

Infiltration-excess Overland Flow

Authors

153

  1. TS
    Tammo S. Steenhuis

    Cornell University, United States

    5 publications · 240 citations

    5

    h-index

  2. FL
    Fred L. Ogden

    University of Wyoming, United States

    4 publications · 374 citations

    4

    h-index

  3. NV
    Nick van de Giesen

    Delft University of Technology, Netherlands

    4 publications · 333 citations

    4

    h-index

  4. RM
    Roger Moussa

    Laboratoire d'étude des Interactions Sol - Agrosystème - Hydrosystème, France

    3 publications · 294 citations

    3

    h-index

  5. TS
    T.J. Stomph

    Wageningen University & Research, Netherlands

    3 publications · 299 citations

    3

    h-index

1–5 of 153

Venues

  1. Hydrological Processes

    15 publications · 1.1K citations

    13

    h-index

  2. Journal of Hydrology

    6 publications · 359 citations

    6

    h-index

  3. Water Resources Research

    6 publications · 545 citations

    6

    h-index

  4. Journal of Hydrologic Engineering

    5 publications · 182 citations

    5

    h-index

  5. Advances in Water Resources

    3 publications · 167 citations

    3

    h-index

1–5