Baroclinic Instability

Baroclinic Instability is a fundamental instability mechanism in atmospheric dynamics whereby horizontal temperature gradients in a rotating, stratified fluid system extract available potential energy to generate transient eddies and large-scale weather systems, distinguishing it from other instabilities by its dependence on the misalignment of pressure and density surfaces.

2.1K

Publications

132.4K

Citations

3.2K

Authors

853

Institutions

Publications per year

2017–2026

237

Authors

3.2K

  1. BJ
    Brian J. Hoskins

    University of Reading, United Kingdom

    30 publications · 4K citations

    23

    h-index

  2. JP
    Joseph Pedlosky

    Woods Hole Oceanographic Institution, United States

    35 publications · 1.6K citations

    22

    h-index

  3. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    25 publications · 2.3K citations

    20

    h-index

  4. PL
    P. L. Read

    University of Oxford, United Kingdom

    28 publications · 891 citations

    19

    h-index

  5. LF
    Lance F. Bosart

    University at Albany, State University of New York, United States

    18 publications · 1.3K citations

    17

    h-index

1–5 of 3.2K

Venues

  1. Journal of the Atmospheric Sciences

    442 publications · 28.3K citations

    87

    h-index

  2. Journal of Physical Oceanography

    308 publications · 18.7K citations

    74

    h-index

  3. Monthly Weather Review

    136 publications · 22K citations

    53

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 111 publications · 6.6K citations

    51

    h-index

  5. 50

    h-index

1–5