Lagrangian approach to geostrophic adjustment of frontal anomalies in a stratified fluid
From MaRDI portal
Publication:3081175
DOI10.1080/03091920512331328080zbMath1206.86027OpenAlexW2099467809MaRDI QIDQ3081175
R. Plougonven, Vladimir Zeitlin
Publication date: 5 March 2011
Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1080/03091920512331328080
Lua error in Module:PublicationMSCList at line 37: attempt to index local 'msc_result' (a nil value).
Related Items (11)
Nonlinear development of inertial instability in a barotropic shear ⋮ On the well-posedness of reduced \(3D\) primitive geostrophic adjustment model with weak dissipation ⋮ Higher-order error estimates for physics-informed neural networks approximating the primitive equations ⋮ The limiting form of inertial instability in geophysical flows ⋮ Trapped symmetric disturbances in rotating shear flows ⋮ Symmetric and asymmetric inertial instability of zonal jets on the -plane with complete Coriolis force ⋮ A study of surface semi-geostrophic turbulence: freely decaying dynamics ⋮ On the effect of rotation on the life-span of analytic solutions to the \(3D\) Inviscid primitive equations ⋮ Hydrostatic approximation of the 2D MHD system in a thin strip with a small analytic data ⋮ Inertial, barotropic, and baroclinic instabilities of the Bickley jet in two-layer rotating shallow water model ⋮ Inertial versus baroclinic instability of the Bickley jet in continuously stratified rotating fluid
Cites Work
- Oblique boundary value problems for equations of Monge-Ampère type
- Generalised Lagrangian Solutions for Atmospheric and Oceanic Flows
- The neumann problem for equations of monge-ampère type
- Frontal geostrophic adjustment, slow manifold and nonlinear wave phenomena in one-dimensional rotating shallow water. Part 1. Theory
- Frontal geostrophic adjustment and nonlinear wave phenomena in one-dimensional rotating shallow water. Part 2. High-resolution numerical simulations
- Wave–vortex interaction in rotating shallow water. Part 1. One space dimension
This page was built for publication: Lagrangian approach to geostrophic adjustment of frontal anomalies in a stratified fluid