On the equatorial Ekman layer
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Publication:4976846
DOI10.1017/jfm.2016.493zbMath1456.76040arXiv1602.08647OpenAlexW3106028384WikidataQ57946369 ScholiaQ57946369MaRDI QIDQ4976846
Andrew M. Soward, Florence Marcotte, Emmanuel Dormy
Publication date: 2 August 2017
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://arxiv.org/abs/1602.08647
Boundary-layer theory, separation and reattachment, higher-order effects (76D10) Geophysical flows (76U60)
Related Items (6)
Spin-down in a rapidly rotating cylinder container with mixed rigid and stress-free boundary conditions ⋮ Stress-driven spin-down of a viscous fluid within a spherical shell ⋮ Mathematical study of the equatorial Ekman boundary layer ⋮ Internal shear layers from librating objects ⋮ Damping effects in boundary layers for rotating fluids with small viscosity ⋮ Stewartson-layer instability in a wide-gap spherical Couette experiment: Rossby number dependence
Uses Software
Cites Work
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- Asymptotic behavior of geophysical fluids in highly rotating balls
- Instabilities of the Stewartson layer. II: Supercritical mode transitions
- The connection between Ekman and Stewartson layers for a rotating disk
- Non-axisymmetric flows in a differential-disk rotating system
- Successive elimination of shear layers by a hierarchy of constraints in inviscid spherical-shell flows
- Inertial waves in a spherical shell induced by librations of the inner sphere: experimental and numerical results
- The almost-rigid rotation of viscous fluid between concentric spheres
- On almost rigid rotations
- Mathematical Aspects of Natural Dynamos
- On the Stability of a Maclaurin Spheroid of Small Viscosity.
- Instabilities of the Stewartson layer Part 1. The dependence on the sign of $Ro$
- A super-rotating shear layer in magnetohydrodynamic spherical Couette flow
- The onset of thermal convection in rotating spherical shells
- On the internal shear layers spawned by the critical regions in oscillatory Ekman boundary layers
- The magneto-hydrodynamics of a rotating fluid and the earth’s dynamo problem
- On almost rigid rotations. Part 2
- Singularities of Hartmann layers
- Pathological oscillations of a rotating fluid
- The structure of free vertical shear layers in a rotating fluid and the motion produced by a slowly rising body
- On the flow properties of a fluid between concentric spheres
- An equatorial boundary layer
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