Terrain-driven Flow

Terrain-Driven Flow is a type of atmospheric boundary-layer flow distinguished by its generation and modification through the interaction of wind with orographic features such as mountains, ridges, and valleys, leading to spatially heterogeneous wind patterns, turbulence, and thermal structures directly imposed by the underlying topography.

45

Publications

1.9K

Citations

160

Authors

92

Institutions

Publications per year

2017–2026

8

Authors

160

  1. NK
    Norbert Kalthoff

    Karlsruhe Institute of Technology, Germany

    2 publications · 117 citations

    2

    h-index

  2. UC
    U. Corsmeier

    Karlsruhe Institute of Technology, Germany

    2 publications · 117 citations

    2

    h-index

  3. DR
    Dale R. Durran

    University of Washington, United States

    2 publications · 125 citations

    2

    h-index

  4. KW
    Keith W. Ayotte

    York University, Canada

    2 publications · 64 citations

    2

    h-index

  5. SG
    S. Gaberšek

    United States Naval Research Laboratory, United States

    2 publications · 96 citations

    2

    h-index

1–5 of 160

Venues

  1. Boundary-Layer Meteorology

    9 publications · 313 citations

    9

    h-index

  2. Monthly Weather Review

    8 publications · 502 citations

    8

    h-index

  3. 5

    h-index

  4. 2

    h-index

  5. Journal of the Atmospheric Sciences

    2 publications · 61 citations

    2

    h-index

1–5