Mountain Inversions

Mountain Inversions is a meteorological phenomenon characterized by a temperature inversion layer that forms within the mountain boundary layer, in which atmospheric temperature increases with altitude due to radiative cooling of mountain surfaces and subsequent cold air pooling in valleys, distinguishing it from free-atmospheric lapse rate patterns.

27

Publications

1.5K

Citations

75

Authors

47

Institutions

Publications per year

2017–2026

8

Variants

Mountain Temperature Inversions

Authors

75

  1. CD
    C. David Whiteman

    University of Utah, United States

    5 publications · 502 citations

    5

    h-index

  2. TB
    Thomas B. McKee

    Colorado State University, United States

    3 publications · 149 citations

    3

    h-index

  3. RM
    Robert M. Banta

    Cooperative Institute for Research in Environmental Sciences, United States

    1 publications · 23 citations

    1

    h-index

  4. MY
    Mohammed Y. Ali

    Khalifa University of Science and Technology, United Arab Emirates

    1 publications · 31 citations

    1

    h-index

  5. YJ
    Yongshun John Chen

    Peking University, China

    1 publications · 93 citations

    1

    h-index

1–5 of 75

Venues

  1. Journal of applied meteorology

    3 publications · 432 citations

    3

    h-index

  2. Journal of the Atmospheric Sciences

    2 publications · 44 citations

    2

    h-index

  3. Theoretical and Applied Climatology

    2 publications · 65 citations

    2

    h-index

  4. Physics of The Earth and Planetary Interiors

    1 publications · 30 citations

    1

    h-index

  5. 1

    h-index

1–5