Linear Baroclinic Instability

Linear Baroclinic Instability is a theoretical framework in atmospheric and oceanic dynamics that describes the growth of small-amplitude perturbations in a baroclinic shear flow through linearized equations of motion, distinguishing it from nonlinear or finite-amplitude instability mechanisms by focusing exclusively on the initial exponential growth phase governed by linear dynamics.

111

Publications

4.8K

Citations

214

Authors

106

Institutions

Publications per year

2017–2026

12

Authors

214

  1. JP
    Joseph Pedlosky

    Woods Hole Oceanographic Institution, United States

    3 publications · 75 citations

    3

    h-index

  2. PL
    P. L. Read

    University of Oxford, United Kingdom

    3 publications · 62 citations

    3

    h-index

  3. RM
    R. M. Samelson

    Oregon State University, United States

    3 publications · 79 citations

    3

    h-index

  4. JE
    John E. Hart

    University of Colorado Boulder, United States

    3 publications · 85 citations

    3

    h-index

  5. RN
    R. N. Keshavamurty

    Indian Institute of Tropical Meteorology, India

    2 publications · 59 citations

    2

    h-index

1–5 of 214

Venues

  1. Journal of the Atmospheric Sciences

    27 publications · 1.2K citations

    19

    h-index

  2. Journal of Physical Oceanography

    16 publications · 477 citations

    13

    h-index

  3. Journal of Fluid Mechanics

    9 publications · 295 citations

    9

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 8 publications · 365 citations

    8

    h-index

  5. 5

    h-index

1–5