The origin of the stationary frontal wave packet spontaneously generated in rotating stratified vortex dipoles
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Publication:5440058
DOI10.1017/S0022112007008816zbMath1151.76622MaRDI QIDQ5440058
Publication date: 31 January 2008
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Vortex flows for incompressible inviscid fluids (76B47) General theory of rotating fluids (76U05) Stratification effects in inviscid fluids (76B70)
Related Items (8)
Piecewise uniform potential vorticity pancake shielded vortices ⋮ Cyclone–anticyclone asymmetry in gravity wave radiation from a co-rotating vortex pair in rotating shallow water ⋮ Isolated marginally stable geophysical vortices ⋮ Balance dynamics in rotating stratified turbulence ⋮ Spontaneous inertia–gravity wave emission in the differentially heated rotating annulus experiment ⋮ Investigation of Boussinesq dynamics using intermediate models based on wave–vortical interactions ⋮ Potential vorticity and inertia–gravity waves ⋮ Multipolar spherical and cylindrical vortices
Cites Work
- Wave-vortex dynamics in rotating shallow water
- Vertical velocity in mesoscale geophysical flows
- A balanced approach to modelling rotating stably stratified geophysical flows
- Optimal potential vorticity balance of geophysical flows
- On the generation mechanisms of short-scale unbalanced modes in rotating two-layer flows with vertical shear
- Gravity wave radiation from vortex trains in rotating shallow water
- Equilibrium dynamics in a forced-dissipative f-plane shallow-water system
- Spiral patterns of inertia–gravity waves in geophysical flows
- Fluctuation growth and instability associated with a singularity of the balance equations
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