On the propagation of hydromagnetic- inertial-gravity waves in magnetic-velocity shear

DOI10.1080/03091927808242642zbMath0417.76068OpenAlexW2014271215WikidataQ114640947 ScholiaQ114640947MaRDI QIDQ3208354

M. El Sawi, I. A. Eltayeb

Publication date: 1978

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

Full work available at URL: https://doi.org/10.1080/03091927808242642

zbMATH Keywords

Boussinesq fluidpropagation propertieshorizontal rotationhydromagnetic critical layershydromagnetic-inertial-gravity waveslatitudinally shearedmagnetic-velocity shearvertically sheared

Mathematics Subject Classification ID

Magnetohydrodynamics and electrohydrodynamics (76W05) Singular perturbations, turning point theory, WKB methods for ordinary differential equations (34E20) Waves and radiation in optics and electromagnetic theory (78A40) Hydrodynamic and hydromagnetic problems in astronomy and astrophysics (85A30)

Cites Work

• Generation of Magnetic Fields by Fluid Motion
• A convection-driven dynamo I. The weak field case
• On finite amplitude convection in a rotating magnetic system
• On double-roll convection in a rotating magnetic system
• Critical-level behaviour and wave amplification of a gravity wave incident upon a shear layer
• Overstable hydromagnetic convection in a rotating fluid layer
• Magnetic field generation by baroclinic waves
• On over-reflexion
• On linear wave motions in magnetic-velocity shears
• Propagation of hydormagnetic planetary waves on a beta-plane through magnetic and velocity shear
• Hydromagnetic convective instability of a rotating, self-gravitating fluid sphere containing a uniform distribution of heat sources
• On hydromagnetic waves in a stratified rotating incompressible fluid
• Wavetrains in Inhomogeneous Moving Media
• Group Velocity
• Hydromagnetic planetary waves
• The critical layer in stratified shear flow
• Hydromagnetic convection in a rapidly rotating fluid layer
• Magnetohydrodynamics of the Earth's Core
• Generation of magnetic fields by convection

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