Thermally Driven Circulations

Thermally Driven Circulations is a meteorological phenomenon in which local winds are generated due to differential heating between mountain and valley surfaces, creating a pressure gradient that drives air movement upslope during the day and downslope at night.

107

Publications

6.5K

Citations

248

Authors

140

Institutions

Publications per year

2017–2026

9

Variants

Thermally Driven Wind Systems

Authors

248

  1. ML
    Manuela Lehner

    University of Utah, United States

    6 publications · 226 citations

    6

    h-index

  2. CD
    C. David Whiteman

    University of Utah, United States

    5 publications · 72 citations

    5

    h-index

  3. HJ
    Harindra J. S. Fernando

    University of Notre Dame, United States

    4 publications · 152 citations

    4

    h-index

  4. MW
    Mathias W. Rotach

    Universität Innsbruck, Austria

    4 publications · 278 citations

    4

    h-index

  5. MS
    M. Segal

    Colorado State University, United States

    4 publications · 766 citations

    4

    h-index

1–5 of 248

Venues

  1. Journal of the Atmospheric Sciences

    14 publications · 2K citations

    13

    h-index

  2. Monthly Weather Review

    11 publications · 756 citations

    10

    h-index

  3. Journal of Applied Meteorology and Climatology

    JAMC · 9 publications · 252 citations

    9

    h-index

  4. 7

    h-index

  5. Journal of Applied Meteorology

    5 publications · 349 citations

    5

    h-index

1–5