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.
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Baroclinic instability in ocean currents
Isidoro Orlanski, Michael D. Cox · Geophysical Fluid Dynamics · 1973 · 111 citations
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Woods Hole Oceanographic Institution
Falmouth, United States
12 h-index
20 publications
923 citations
Massachusetts Institute of Technology
Cambridge, United States
8 h-index
9 publications
297 citations
University of California, Los Angeles
Los Angeles, United States
6 h-index
11 publications
489 citations

University of Oslo
Oslo, Norway
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7 publications
195 citations
École Polytechnique
Palaiseau, France
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4 publications
70 citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
3 h-index
4 publications
194 citations

Imperial College London
London, United Kingdom
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4 publications
131 citations
Laboratoire de Météorologie Dynamique
Palaiseau, France
3 h-index
7 publications
126 citations
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41 publications · 1.4K citations
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JGR · 13 publications · 592 citations
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