Instability of coupled geostrophic density fronts and its nonlinear evolution
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Publication:5302713
DOI10.1017/S0022112008003145zbMath1151.76486MaRDI QIDQ5302713
Emilie Scherer, Vladimir Zeitlin
Publication date: 8 January 2009
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Hydrology, hydrography, oceanography (86A05) General theory of rotating fluids (76U05) Stability and instability of geophysical and astrophysical flows (76E20)
Related Items (3)
Nonlinear development of inertial instability in a barotropic shear ⋮ Instabilities of buoyancy-driven coastal currents and their nonlinear evolution in the two-layer rotating shallow-water model. Part 1. Passive lower layer ⋮ Instabilities of buoyancy-driven coastal currents and their nonlinear evolution in the two-layer rotating shallow water model. Part 2. Active lower layer
Uses Software
Cites Work
- Unnamed Item
- Nonlinear theory of geostrophic adjustment. Part 1. Rotating shallow-water model
- General stability conditions for zonal flows in a one-layer model on the β-plane or the sphere
- Long-wave instability of an isolated front
- Stable and unstable shear modes of rotating parallel flows in shallow water
- On the stability of elliptical vortex solutions of the shallow-water equations
- Rossby-Kelvin instability: a new type of ageostrophic instability caused by a resonance between Rossby waves and gravity waves
- Ageostrophic instability of ocean currents
- A nonlinear critical layer generated by the interaction of free Rossby waves
- Spectral Methods in MATLAB
- A Fast and Stable Well-Balanced Scheme with Hydrostatic Reconstruction for Shallow Water Flows
- Frontal geostrophic adjustment and nonlinear wave phenomena in one-dimensional rotating shallow water. Part 2. High-resolution numerical simulations
- Stability of linear shear flows in shallow water
- Breaking of balanced and unbalanced equatorial waves
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