Baroclinic Structure

Baroclinic Structure is a theoretical construct in atmospheric dynamics characterized by the misalignment between pressure and density surfaces, which enables the generation and evolution of weather systems through the conversion of potential energy into kinetic energy via horizontal temperature gradients.

1.5K

Publications

98.2K

Citations

3K

Authors

765

Institutions

Publications per year

2017–2026

194

Authors

3K

  1. LF
    Lance F. Bosart

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

    17 publications · 1.1K citations

    15

    h-index

  2. BD
    Boris Dewitte

    Laboratoire d’Études en Géophysique et Océanographie Spatiales, France

    13 publications · 592 citations

    13

    h-index

  3. PL
    P. L. Read

    University of Oxford, United Kingdom

    12 publications · 307 citations

    12

    h-index

  4. DR
    D. Randolph Watts

    University of Rhode Island, United States

    11 publications · 340 citations

    11

    h-index

  5. RJ
    Richard J. Greatbatch

    GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany

    10 publications · 306 citations

    10

    h-index

1–5 of 3K

Venues

  1. Journal of Physical Oceanography

    210 publications · 13.8K citations

    64

    h-index

  2. Journal of the Atmospheric Sciences

    206 publications · 12.1K citations

    58

    h-index

  3. Monthly Weather Review

    143 publications · 22.3K citations

    56

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 140 publications · 8.8K citations

    55

    h-index

  5. Journal of Climate

    73 publications · 6.4K citations

    42

    h-index

1–5