The rectification of wind-driven flow due to its instabilities

Keyphrases

• Lower Layer 100%
• Weakly Nonlinear Analysis 100%
• Wind-driven Flow 100%
• Numerical Model 50%
• Layer Thickness 50%
• Friction 50%
• Eddy-resolving 50%
• Vorticity 50%
• Unstable Modes 50%
• Baroclinic Instability 50%
• Barotropic 50%
• Time Dependence 50%
• Hopf Bifurcation 50%
• Wind-driven Ocean Circulation 50%
• Self-interaction 50%
• Geostrophic 50%
• Lateral Friction 50%
• Quasi-geostrophic 50%
• Interfacial Friction 50%
• Double Gyre 50%
• Deep Flow 50%
• Supercritical Condition 50%
• Reynolds Stress 50%
• Phase-lag 50%
• Deep Circulation 50%
• Two-layer Model 50%
• Picture-based 50%
• Dependent View 50%

Engineering

• Driven Flow 100%
• Nonlinear Analysis 100%
• Rectification 100%
• Layer Thickness 50%
• Oscillatory 50%
• Layer Model 50%
• Critical Condition 50%
• Vorticity 50%
• Reynolds Stress 50%
• Phase Lag 50%
• Supercritical Condition 50%
• Numerical Model 50%
• Hopf Bifurcation 50%
• Baroclinic Instability 50%

Earth and Planetary Sciences

• Bifurcation 100%
• Ocean Circulation 100%
• Numerical Model 100%
• Rectification 100%
• Baroclinic Instability 100%
• Time Dependence 100%