Katabatic Wind Formation

Katabatic Wind Formation is a meteorological phenomenon characterized by the generation of downslope winds due to the gravitational flow of cold, dense air masses originating from elevated cooling surfaces, distinguishing it from other wind formation mechanisms by its thermally driven, topographically channeled descent.

35

Publications

1.5K

Citations

109

Authors

54

Institutions

Publications per year

2017–2026

2

Authors

109

  1. DH
    David H. Bromwich

    The Ohio State University, United States

    3 publications · 373 citations

    3

    h-index

  2. TR
    Thomas R. Parish

    University of Wyoming, United States

    2 publications · 100 citations

    2

    h-index

  3. JB
    J.G. Bartzis

    National Centre of Scientific Research "Demokritos", Greece

    2 publications · 38 citations

    2

    h-index

  4. KP
    Kyriakos Papadopoulos

    National Centre of Scientific Research "Demokritos", Greece

    2 publications · 82 citations

    2

    h-index

  5. GH
    Günther Heinemann

    Universität Trier, Germany

    2 publications · 130 citations

    2

    h-index

1–5 of 109

Venues

  1. Boundary-Layer Meteorology

    6 publications · 235 citations

    6

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 296 citations

    3

    h-index

  3. Monthly Weather Review

    3 publications · 168 citations

    3

    h-index

  4. Acta Geophysica

    2 publications · 53 citations

    2

    h-index

  5. Tellus A Dynamic Meteorology and Oceanography

    2 publications · 35 citations

    2

    h-index

1–5