Mountain Climate Forcing

Mountain Climate Forcing is a geophysical mechanism that denotes the aggregate influence of orographic features on atmospheric processes, whereby topographic elevation, slope, and aspect differentially modify incident solar radiation, temperature gradients, wind patterns, and precipitation distribution relative to surrounding lowlands.

145

Publications

12.4K

Citations

550

Authors

278

Institutions

Publications per year

2017–2026

51

Authors

550

  1. GW
    Guoxiong Wu

    Institute of Atmospheric Physics, China

    11 publications · 1.5K citations

    11

    h-index

  2. YL
    Yimin Liu

    Institute of Atmospheric Physics, China

    9 publications · 1K citations

    9

    h-index

  3. AD
    Anmin Duan

    Institute of Atmospheric Physics, China

    7 publications · 1.2K citations

    7

    h-index

  4. DA
    Duan Anmin

    Chinese Academy of Sciences, China

    3 publications · 89 citations

    3

    h-index

  5. BH
    Bian He

    Chinese Academy of Sciences, China

    3 publications · 156 citations

    3

    h-index

1–5 of 550

Venues

  1. Climate Dynamics

    13 publications · 1.4K citations

    13

    h-index

  2. Geology

    9 publications · 1.1K citations

    9

    h-index

  3. Earth and Planetary Science Letters

    8 publications · 628 citations

    8

    h-index

  4. Theoretical and Applied Climatology

    4 publications · 69 citations

    4

    h-index

  5. Quaternary Science Reviews

    4 publications · 88 citations

    4

    h-index

1–5