On the collision between deep anticyclones and seamounts
DOI10.1016/S0997-7546(01)01124-4zbMath1011.76094OpenAlexW2120730471MaRDI QIDQ5950216
Publication date: 6 December 2001
Published in: European Journal of Mechanics. B. Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/s0997-7546(01)01124-4
collisionArakawa finite difference schemedeep topographically-steered anticyclonic eddiesfinite-amplitude height variationspotential vorticity equationseamountssecond-order leapfrog proceduresub-inertial baroclinic dynamicstopographic vorticity gradienttwo-layer intermediate length-scale model
Hydrology, hydrography, oceanography (86A05) Finite difference methods applied to problems in fluid mechanics (76M20) General theory of rotating fluids (76U05)
Cites Work
- Unnamed Item
- Computational design for long-term numerical integration of the equations of fluid motion: two-dimensional incompressible flow. Part I
- A unified asymptotic derivation of two-layer, frontal geostrophic models including planetary sphericity and variable topography
- Coherent baroclinic eddies on a sloping bottom
- Eddy formation by dense flows on slopes in a rotating fluid
- Dynamics of radiating cold domes on a sloping bottom
- Sub-inertial dynamics of density-driven flows in a continuously stratified fluid on a sloping bottom. I. Model derivation and stability characteristics
- Sub–inertial dynamics of density–driven flows in a continuously stratified fluid on a sloping bottom. II. Isolated eddies and radiating cold domes
- Nonlinear stability of intermediate baroclinic flow on a sloping bottom
- On the baroclinic instability of axisymmetric rotating gravity currents with bottom slope
- On the baroclinic instability of cold-core coupled density fronts on a sloping continental shelf
- Dynamics of ventilated coherent cold eddies on a sloping bottom
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