Oceanic Jet Instability

Oceanic Jet Instability is a barotropic instability mechanism characterized by the hydrodynamic instability of zonally oriented ocean currents due to shear-driven perturbations in the absence of horizontal density gradients, distinguished from other jet instabilities by its reliance on the vertical structure of the flow and the beta effect in rotating shallow-water systems.

106

Publications

3.9K

Citations

209

Authors

108

Institutions

Publications per year

2017–2026

3

Authors

209

  1. GR
    Glenn R. Flierl

    Massachusetts Institute of Technology, United States

    6 publications · 156 citations

    6

    h-index

  2. MG
    Michael Ghil

    University of California, Los Angeles, United States

    5 publications · 192 citations

    5

    h-index

  3. MS
    M. Susan Lozier

    Duke University, United States

    3 publications · 99 citations

    3

    h-index

  4. IK
    Igor Kamenkovich

    University of Miami, United States

    3 publications · 150 citations

    3

    h-index

  5. YF
    Yizhak Feliks

    Israel Institute for Biological Research, Israel

    3 publications · 92 citations

    3

    h-index

1–5 of 209

Venues

  1. Journal of Physical Oceanography

    41 publications · 1.4K citations

    23

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 13 publications · 592 citations

    12

    h-index

  3. Journal of Fluid Mechanics

    6 publications · 237 citations

    6

    h-index

  4. Journal of the Atmospheric Sciences

    6 publications · 422 citations

    6

    h-index

  5. Tellus A Dynamic Meteorology and Oceanography

    5 publications · 56 citations

    5

    h-index

1–5