A wave amplitude transition in a quasi-linear model with radiative forcing and surface drag

Keyphrases

• Mean Flow 100%
• Radiative Forcing 100%
• Surface Drag 100%
• Quasi-linear Model 100%
• Wave Amplitude 100%
• Baroclinic 60%
• Equilibration 40%
• Two-layer 40%
• Quasi-linear 40%
• Barotropic 40%
• Vertical Shear 40%
• Potential Vorticity 40%
• Parameter Values 20%
• Large Amplitude 20%
• Zonal Wavenumber 20%
• Equilibrium State 20%
• Growth Rate 20%
• Bifurcation 20%
• Quasi-geostrophic 20%
• Meaning Potential 20%
• Rossby Deformation Radius 20%
• Radiative Equilibrium 20%
• Finite-amplitude Waves 20%
• Newtonian Heating 20%
• Critical Failure Surface 20%
• Wave-induced 20%
• Finite Amplitude 20%
• Destabilization Mechanism 20%
• Plane Model 20%
• Weak Instability 20%
• Frictional Damping 20%
• Upper Layer 20%
• Baroclinic Jet 20%
• Radiative Damping 20%
• Flow Potential 20%
• Upper Tropospheric Jet 20%
• Model Evolution 20%
• Ekman Damping 20%

Earth and Planetary Sciences

• Radiative Forcing 100%
• Destabilization 100%
• Critical Level 66%
• Potential Flow 33%