Rain Shadow Effects

Rain Shadow Effects is a climatological phenomenon in which a mountain range causes a significant reduction in precipitation on its leeward side, resulting in drier conditions relative to the windward side due to orographic lifting and subsequent moisture depletion of air masses.

80

Publications

4K

Citations

272

Authors

121

Institutions

Publications per year

2017–2026

23

Variants

Rain ShadowRain Shadow Effect

Authors

272

  1. CP
    C. Page Chamberlain

    Stanford University, United States

    4 publications · 348 citations

    4

    h-index

  2. DR
    Dale R. Durran

    University of Washington, United States

    3 publications · 97 citations

    3

    h-index

  3. SB
    S. B. Morwal

    Indian Institute of Tropical Meteorology, India

    3 publications · 55 citations

    3

    h-index

  4. RS
    R. S. Maheskumar

    Indian Institute of Tropical Meteorology, India

    3 publications · 55 citations

    3

    h-index

  5. SG
    S. G. Narkhedkar

    Indian Institute of Tropical Meteorology, India

    3 publications · 55 citations

    3

    h-index

1–5 of 272

Venues

  1. Journal of Hydrometeorology

    4 publications · 384 citations

    4

    h-index

  2. Climate Dynamics

    3 publications · 82 citations

    3

    h-index

  3. Annals of Glaciology

    2 publications · 45 citations

    2

    h-index

  4. Australian Journal of Botany

    AJB · 2 publications · 47 citations

    2

    h-index

  5. Arctic and Alpine Research

    2 publications · 24 citations

    2

    h-index

1–5