Anabatic Winds

Anabatic Wind is a thermally driven upslope breeze that occurs when solar heating warms mountain slopes, causing the adjacent air to rise due to density differences, distinguishing it from katabatic and other wind types by its daytime occurrence and upward trajectory along terrain.

19

Publications

899

Citations

66

Authors

37

Institutions

Publications per year

2017–2026

2

Authors

66

  1. IM
    I. M. Avruch

    Netherlands Institute for Radio Astronomy, Netherlands

    1 publications · 234 citations

    1

    h-index

  2. MK
    M. K. Bird

    University of Bonn, Germany

    1 publications · 234 citations

    1

    h-index

  3. GL
    G. L. Tyler

    Stanford University, United States

    1 publications · 234 citations

    1

    h-index

  4. LG
    Leonid Gurvits

    Joint Institute for VLBI ERIC, Netherlands

    1 publications · 234 citations

    1

    h-index

  5. DH
    D. H. Atkinson

    University of Idaho, United States

    1 publications · 234 citations

    1

    h-index

1–5 of 66

Venues

  1. Monthly Weather Review

    3 publications · 88 citations

    3

    h-index

  2. 2

    h-index

  3. Nature

    1 publications · 234 citations

    1

    h-index

  4. npj Climate and Atmospheric Science

    1 publications · 95 citations

    1

    h-index

  5. Atmospheric chemistry and physics

    1 publications · 78 citations

    1

    h-index

1–5