Abstract
Equilibration of two-dimensional Eady waves is numerically investigated using the geostrophic momentum equations incorporating heat and momentum diffusion. Extended solutions are obtained beyond what would be the collapse of surface fronts in the inviscid theory, and are found to accurately reproduce the equilibration of baroclinic waves simulated with the primitive equations. Potential vorticity anomalies produced at the surface fronts are essential in the initial amplitude saturation and in the asymptotic behavior of the equilibrated flow. A supergeostrophic shear spun up nonlinearly in the zonal flow also plays an important role in causing the reversal of the tilt. -from Author
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CITATION STYLE
Nakamura, N. (1994). Nonlinear equilibration of two-dimensional Eady waves: simulations with viscous geostrophic momentum equations. Journal of the Atmospheric Sciences, 51(7), 1023–1035. https://doi.org/10.1175/1520-0469(1994)051<1023:NEOTDE>2.0.CO;2
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