Complex Terrain Flow

Complex Terrain Flow is a fluid dynamics phenomenon characterized by the three-dimensional distortion and acceleration of wind flow due to the interaction of atmospheric boundary layer winds with irregular topographic features such as mountains, valleys, and escarpments.

477

Publications

22.3K

Citations

1.4K

Authors

478

Institutions

Publications per year

2017–2026

142

Authors

1.4K

  1. TU
    Takanori Uchida

    Kyushu University, Japan

    13 publications · 351 citations

    13

    h-index

  2. JM
    Jakob Mann

    Technical University of Denmark, Denmark

    15 publications · 960 citations

    13

    h-index

  3. JK
    Julie K. Lundquist

    University of Colorado Boulder, United States

    10 publications · 920 citations

    10

    h-index

  4. FK
    Fotini Katopodes Chow

    University of California, Berkeley, United States

    9 publications · 961 citations

    9

    h-index

  5. MW
    Mathias W. Rotach

    Universität Innsbruck, Austria

    9 publications · 816 citations

    9

    h-index

1–5 of 1.4K

Venues

  1. Boundary-Layer Meteorology

    41 publications · 2K citations

    25

    h-index

  2. 21

    h-index

  3. Monthly Weather Review

    28 publications · 1.5K citations

    20

    h-index

  4. Journal of Applied Meteorology

    23 publications · 985 citations

    17

    h-index

  5. 16

    h-index

1–5