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The geography of linear baroclinic instability in Earth's oceans
K. Shafer Smith
Mathematics
Center for Prototype Climate Modeling
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Keyphrases
Maximum Growth
100%
Eddy Activity
50%
Energetic Conversion
50%
Local Linear Stability Analysis
50%
Energy Conversion Rate
50%
Oceanic Eddies
50%
Stability Calculation
50%
Surface Instability
50%
Eady Growth Rate
50%
Instability Theory
50%
Neutral Density
50%
Earth and Planetary Sciences
Oceanic Circulation
100%