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A wave amplitude transition in a quasi-linear model with radiative forcing and surface drag
Orli Lachmy
, Nili Harnik
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Dive into the research topics of 'A wave amplitude transition in a quasi-linear model with radiative forcing and surface drag'. Together they form a unique fingerprint.
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Keyphrases
Baroclinic
60%
Baroclinic Jet
20%
Barotropic
40%
Bifurcation
20%
Critical Failure Surface
20%
Destabilization Mechanism
20%
Ekman Damping
20%
Equilibration
40%
Equilibrium State
20%
Finite Amplitude
20%
Finite-amplitude Waves
20%
Flow Potential
20%
Frictional Damping
20%
Growth Rate
20%
Large Amplitude
20%
Mean Flow
100%
Meaning Potential
20%
Model Evolution
20%
Newtonian Heating
20%
Parameter Values
20%
Plane Model
20%
Potential Vorticity
40%
Quasi-geostrophic
20%
Quasi-linear
40%
Quasi-linear Model
100%
Radiative Damping
20%
Radiative Equilibrium
20%
Radiative Forcing
100%
Rossby Deformation Radius
20%
Surface Drag
100%
Two-layer
40%
Upper Layer
20%
Upper Tropospheric Jet
20%
Vertical Shear
40%
Wave Amplitude
100%
Wave-induced
20%
Weak Instability
20%
Zonal Wavenumber
20%
Earth and Planetary Sciences
Critical Level
66%
Destabilization
100%
Potential Flow
33%
Radiative Forcing
100%