Foehn Effects

Foehn Effects is a meteorological phenomenon characterized by the warming and drying of air masses descending on the leeward side of mountain ranges, resulting from adiabatic compression following orographic ascent and precipitation on the windward side.

44

Publications

2K

Citations

200

Authors

118

Institutions

Publications per year

2017–2026

20

Variants

Foehn EffectFöhn EffectFöhn Effects

Authors

200

  1. HK
    Hiroyuki Kusaka

    University of Tsukuba, Japan

    3 publications · 113 citations

    3

    h-index

  2. JW
    Jonathan Wille

    Institut des Géosciences de l'Environnement, France

    3 publications · 200 citations

    3

    h-index

  3. JK
    John King

    British Antarctic Survey, United Kingdom

    2 publications · 124 citations

    2

    h-index

  4. ME
    Marcelo E. Seluchi

    Instituto Nacional de Pesquisas Espaciais, Brazil

    2 publications · 208 citations

    2

    h-index

  5. RR
    Raúl R. Cordero

    Universidad de Santiago de Chile, Chile

    2 publications · 134 citations

    2

    h-index

1–5 of 200

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 5 publications · 324 citations

    5

    h-index

  2. Journal of Climate

    4 publications · 294 citations

    4

    h-index

  3. Monthly Weather Review

    3 publications · 161 citations

    3

    h-index

  4. SOLA

    2 publications · 41 citations

    2

    h-index

  5. 2

    h-index

1–5