Temperature Gradient Forcing

Temperature Gradient Forcing is a meteorological mechanism that belongs to the class of atmospheric forcing processes, differentially characterized by the induction of anabatic winds through the localized heating contrast between a sloped surface and the adjacent air layer, thereby generating upward-directed buoyancy-driven airflow.

181

Publications

8.1K

Citations

513

Authors

244

Institutions

Publications per year

2017–2026

21

Authors

513

  1. AH
    Adam H. Sobel

    Columbia University, United States

    6 publications · 1.1K citations

    6

    h-index

  2. WH
    W. Horton

    The University of Texas at Austin, United States

    5 publications · 215 citations

    5

    h-index

  3. KE
    Kerry Emanuel

    Massachusetts Institute of Technology, United States

    4 publications · 161 citations

    4

    h-index

  4. HN
    H. Nordman

    Chalmers University of Technology, Sweden

    3 publications · 67 citations

    3

    h-index

  5. GL
    G. Lebon

    University of Liège, Belgium

    3 publications · 108 citations

    3

    h-index

1–5 of 513

Venues

  1. Physical Review Letters

    PRL · 11 publications · 817 citations

    11

    h-index

  2. Journal of the Atmospheric Sciences

    11 publications · 1.3K citations

    10

    h-index

  3. Journal of Climate

    9 publications · 478 citations

    9

    h-index

  4. Nuclear Fusion

    9 publications · 290 citations

    9

    h-index

  5. Physics of Plasmas

    7 publications · 280 citations

    8

    h-index

1–5