Baroclinic Waves

Baroclinic Waves is a dynamical construct in synoptic-scale atmospheric dynamics representing large-scale instabilities in the baroclinic zone that emerge under quasi-geostrophic balance, distinguished by their generation and propagation due to horizontal temperature gradients and vertical wind shear in a rotating stratified fluid.

1.9K

Publications

110.1K

Citations

3.1K

Authors

754

Institutions

Publications per year

2017–2026

177

Authors

3.1K

  1. BJ
    Brian J. Hoskins

    University of Reading, United Kingdom

    30 publications · 8.3K citations

    26

    h-index

  2. JP
    Joseph Pedlosky

    Woods Hole Oceanographic Institution, United States

    37 publications · 1.4K citations

    21

    h-index

  3. PL
    P. L. Read

    University of Oxford, United Kingdom

    20 publications · 642 citations

    16

    h-index

  4. CS
    Chris Snyder

    NSF National Center for Atmospheric Research, United States

    14 publications · 1.3K citations

    14

    h-index

  5. FZ
    Fuqing Zhang

    Pennsylvania State University, United States

    13 publications · 1.3K citations

    13

    h-index

1–5 of 3.1K

Venues

  1. Journal of the Atmospheric Sciences

    431 publications · 31.1K citations

    87

    h-index

  2. Journal of Physical Oceanography

    301 publications · 15.1K citations

    69

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 161 publications · 10.9K citations

    63

    h-index

  4. Monthly Weather Review

    91 publications · 5K citations

    44

    h-index

  5. 41

    h-index

1–5