Control of baroclinic instability by submesoscale topography
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Publication:5243566
DOI10.1017/jfm.2019.826zbMath1430.76193OpenAlexW2989559944WikidataQ126822532 ScholiaQ126822532MaRDI QIDQ5243566
Publication date: 19 November 2019
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/jfm.2019.826
Hydrology, hydrography, oceanography (86A05) General theory of rotating fluids (76U05) Stability and instability of geophysical and astrophysical flows (76E20)
Related Items (5)
A generalized theory of flow forcing by rough topography ⋮ Spin-down of a baroclinic vortex by irregular small-scale topography ⋮ Spin-down of a barotropic vortex by irregular small-scale topography ⋮ The sandpaper theory of flow–topography interaction for homogeneous shallow-water systems ⋮ Linear stability analysis for flows over sinusoidal bottom topography
Cites Work
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- Eddy viscosity of cellular flows
- Investigation of the stability of a stationary solution of a system of equations for the plane movement of an incompressible viscous liquid
- Enhanced dissipation for quasi-geostrophic motion over small-scale topography
- Atmospheric and Oceanic Fluid Dynamics
- Thermohaline layering on the microscale
- Stratified Kolmogorov flow. Part 2
- Nonlinear dynamics over rough topography: homogeneous and stratified quasi-geostrophic theory
- Eddy viscosity of three-dimensional flow
- On the generation of large-scale eddy-driven patterns: the average eddy model
- Submesoscale currents in the ocean
- Stability of \(\beta\)-plane Kolmogorov flow
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