Quasi-geostrophic turbulence in a rotating homogeneous fluid

DOI10.1080/03091928008241179zbMath0505.76114OpenAlexW2073603277WikidataQ114640807 ScholiaQ114640807MaRDI QIDQ4742484

Alain Colin de Verdière

Publication date: 1980

Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1080/03091928008241179

zbMATH Keywords

rotating cylinderquasi-two-dimensionalgeostrophic contoursEkman spin-up timehomogeneous distribution of bottom sources and sinks which oscillatelarge scale topographiesReynolds numbers 2000

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) General theory of rotating fluids (76U05) Turbulence (76F99)

Related Items (4)

Effects of mesoscale turbulence on the wind-driven circulation in a closed basin with topography ⋮ Quasi-2D Turbulence in Shallow Fluid Layers ⋮ The three-dimensional vortical nature of atmospheric and oceanic turbulent flows ⋮ Why, how, and when, MHD turbulence becomes two-dimensional

Cites Work

• Unnamed Item
• Decay of two-dimensional homogeneous turbulence
• The ‘sliced-cylinder’ laboratory model of the wind-driven ocean circulation. Part 2. Oscillatory forcing and Rossby wave resonance
• Waves and turbulence on a beta-plane
• A simple laboratory model for the oceanic circulation

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