Linear Barotropic Instability

Linear Barotropic Instability is a theoretical framework in geophysical fluid dynamics that characterizes the inherent instability of large-scale atmospheric or oceanic flows on a beta plane under the assumption of no vertical shear, where perturbations grow exponentially due to the interaction between the meridional gradient of the background vorticity and the wave-like disturbances constrained to a single vertical mode.

65

Publications

2.6K

Citations

127

Authors

78

Institutions

Publications per year

2017–2026

4

Authors

127

  1. JP
    Joseph Pedlosky

    Woods Hole Oceanographic Institution, United States

    3 publications · 89 citations

    3

    h-index

  2. JC
    James C. McWilliams

    University of California, Los Angeles, United States

    3 publications · 276 citations

    3

    h-index

  3. IM
    Isaac M. Held

    NOAA Geophysical Fluid Dynamics Laboratory, United States

    2 publications · 85 citations

    2

    h-index

  4. MA
    Michael A. Spall

    Woods Hole Oceanographic Institution, United States

    2 publications · 49 citations

    2

    h-index

  5. SK
    Saroj K. Mishra

    Indian Institute of Technology Delhi, India

    2 publications · 34 citations

    2

    h-index

1–5 of 127

Venues

  1. Journal of the Atmospheric Sciences

    23 publications · 861 citations

    18

    h-index

  2. Journal of Physical Oceanography

    8 publications · 274 citations

    8

    h-index

  3. Journal of Fluid Mechanics

    6 publications · 201 citations

    6

    h-index

  4. 2

    h-index

  5. Geophysical & Astrophysical Fluid Dynamics

    2 publications · 158 citations

    2

    h-index

1–5