On magnetostrophic inertia-less waves in quasi-geostrophic models of planetary cores
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Publication:5879702
DOI10.1080/03091929.2015.1094569OpenAlexW1820374732WikidataQ114640168 ScholiaQ114640168MaRDI QIDQ5879702
Publication date: 2 March 2023
Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1080/03091929.2015.1094569
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Cites Work
- On inertial waves in a rotating fluid sphere
- Deep two-dimensional turbulence: An idealized model for atmospheric jets of the giant outer planets
- Quasigeostrophic model of the instabilities of the Stewartson layer in flat and depth-varying containers
- The magneto-hydrodynamics of a rotating fluid and the earth’s dynamo problem
- The quasi-geostrophic model for rapidly rotating spherical convection outside the tangent cylinder
- Hydromagnetic planetary waves
- On hydromagnetic oscillations in a rotating cavity
- On the theory of core-mantle coupling
- On magnetostrophic mean-field solutions of the geodynamo equations
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