The breakdown of large-scale flows in rotating, stratified fluids
From MaRDI portal
Publication:5755950
DOI10.1063/1.869844zbMath1185.86016OpenAlexW2075843156MaRDI QIDQ5755950
James C. McWilliams, Irad Yavneh, Peter R. Gent, Michael John Priestley Cullen
Publication date: 15 August 2007
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.869844
Related Items
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, Submesoscale baroclinic instability in the balance equations, Submesoscale surface fronts and filaments: secondary circulation, buoyancy flux, and frontogenesis, Damping and pumping of a vortex Rossby wave in a monotonic cyclone: Critical layer stirring versus inertia–buoyancy wave emission, Ageostrophic, anticyclonic instability of a geostrophic, barotropic boundary current, Ageostrophic instability in a rotating stratified interior jet, Ageostrophic instability in rotating shallow water
Cites Work
- The dynamics of enstrophy transfer in two-dimensional hydrodynamics
- A numerical model of the balance equations in a periodic domain and an example of balanced turbulence
- Instability of an axisymmetric vortex in a stably stratified, rotating environment
- Notes on the mean value property for certain degenerate elliptic operators
- Multigrid solution of rotating, stably stratified flows: The balance equations and their turbulent dynamics
- Hamiltonian balance equations
- Groups of diffeomorphisms and the motion of an incompressible fluid
- Interior estimates for elliptic systems of partial differential equations
- ON TYPES OF DEGENERATE ELLIPTIC OPERATORS
- New equations for nearly geostrophic flow
- Evolution of wavelike disturbances in shear flows : a class of exact solutions of the Navier-Stokes equations
- The modified cuinulant expansion for two-dimensional isotropic turbulence
- Evidence for a singularity of the three-dimensional, incompressible Euler equations
- Elliptical instability in a stably stratified rotating fluid
