Orographic Rainfall

Orographic Rainfall is a type of precipitation that results from the adiabatic cooling and condensation of moist air masses as they are forced to ascend over elevated terrain, distinguishing it from other rainfall mechanisms by its direct dependence on topographic uplift.

310

Publications

21.5K

Citations

770

Authors

375

Institutions

Publications per year

2017–2026

53

Authors

770

  1. YL
    Yuh‐Lang Lin

    North Carolina State University, United States

    10 publications · 605 citations

    10

    h-index

  2. RB
    Ronald B. Smith

    Yale University, United States

    9 publications · 883 citations

    9

    h-index

  3. AP
    Ana P. Barros

    Duke University, United States

    8 publications · 556 citations

    8

    h-index

  4. RR
    Richard Rotunno

    NSF National Center for Atmospheric Research, United States

    6 publications · 752 citations

    6

    h-index

  5. IB
    Idar Barstad

    Bjerknes Centre for Climate Research, Norway

    6 publications · 585 citations

    6

    h-index

1–5 of 770

Venues

  1. 26

    h-index

  2. Monthly Weather Review

    28 publications · 1.6K citations

    25

    h-index

  3. Journal of the Atmospheric Sciences

    18 publications · 1.7K citations

    17

    h-index

  4. Atmospheric Research

    16 publications · 530 citations

    16

    h-index

  5. Journal of Hydrometeorology

    14 publications · 823 citations

    14

    h-index

1–5