Balanced and unbalanced routes to dissipation in an equilibrated Eady flow
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Publication:3586968
DOI10.1017/S0022112009993272zbMath1193.76065MaRDI QIDQ3586968
James C. McWilliams, M. Jeroen Molemaker, Xavier Capet
Publication date: 1 September 2010
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Related Items (13)
Spontaneous inertia-gravity-wave generation by surface-intensified turbulence ⋮ Instability of a periodic flow in geostrophic and hydrostatic balance ⋮ The emergence of fast oscillations in a reduced primitive equation model and its implications for closure theories ⋮ Spontaneous imbalance in the non-hydrostatic Boussinesq equations ⋮ Transport and emergent stratification in the equilibrated Eady model: the vortex-gas scaling regime ⋮ Energy-conserving Galerkin approximations for quasigeostrophic dynamics ⋮ The route to dissipation in strongly stratified and rotating flows ⋮ A perturbation approach to understanding the effects of turbulence on frontogenesis ⋮ The role of mixed-layer instabilities in submesoscale turbulence ⋮ Stratified turbulence at the buoyancy scale ⋮ On the effects of frontogenetic strain on symmetric instability and inertia–gravity waves ⋮ Layering and turbulence surrounding an anticyclonic oceanic vortex: in situ observations and quasi-geostrophic numerical simulations ⋮ Inertial instability of intense stratified anticyclones. Part 2. Laboratory experiments
Cites Work
- A stable and accurate convective modelling procedure based on quadratic upstream interpolation
- The transition from geostrophic to stratified turbulence
- Surface kinetic energy transfer in surface quasi-geostrophic flows
- Local balance and cross-scale flux of available potential energy
- Homogenization of potential vorticity in planetary gyres
- Surface quasi-geostrophic dynamics
- Available potential energy and mixing in density-stratified fluids
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