Transient Lateral Flow

Transient Lateral Flow is a hydrological process denoting the temporary, downslope movement of water within the subsurface soil or regolith layer, driven by transient saturation conditions during and immediately following storm events.

25

Publications

829

Citations

58

Authors

45

Institutions

Publications per year

2017–2026

3

Authors

58

  1. JM
    Jean Moureh

    Université Claude Bernard Lyon 1, France

    4 publications · 87 citations

    4

    h-index

  2. MY
    Mourad Yataghene

    Centre National de la Recherche Scientifique, France

    3 publications · 69 citations

    3

    h-index

  3. JR
    J. R. McAfee

    National Oceanic and Atmospheric Administration, United States

    2 publications · 78 citations

    2

    h-index

  4. CD
    Christiaan Dirksen

    U.S. Salinity Laboratory, United States

    1 publications · 14 citations

    1

    h-index

  5. RJ
    R. J. Phillips

    Southwest Research Institute, United States

    1 publications · 63 citations

    1

    h-index

1–5 of 58

Venues

  1. Geophysical Research Letters

    3 publications · 110 citations

    3

    h-index

  2. Planetary and Space Science

    2 publications · 78 citations

    2

    h-index

  3. Water Resources Research

    2 publications · 62 citations

    2

    h-index

  4. Experimental Thermal and Fluid Science

    ETFS · 1 publications · 22 citations

    1

    h-index

  5. 1

    h-index

1–5