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Journal ArticleDOI

Taylor columns between concentric spheres

R. Schopp, +1 more
- 01 Sep 1997 - 
- Vol. 86, Iss: 1, pp 43-73
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TLDR
In this paper, the motion of fluid contained between two concentric spherical surfaces is analyzed in the limit of strong rotation appropriate to large scale flows and arbitrary gap width, and the dynamical equations are written in the natural cylindrical co-ordinate system that gives a central role to the axis of rotation.
Abstract
The motion of fluid contained between two concentric spherical surfaces is analysed in the limit of strong rotation appropriate to large scale flows and arbitrary gap width. To do so, the dynamical equations are written in the natural cylindrical co-ordinate system that gives a central role to the axis of rotation. The case of a homogeneous fluid allows us to give a general solution of the inviscid, steady flow when sources and sinks have prescribed boundary distributions. Fluid can cross the equatorial plane without breaking rotational constraints provided the source-sink forcing is antisymmetric. However the cylindrical surface tangent to the inner sphere at the equator is singular and calls for higher order inertial and/or viscous effects. No specific solution is obtained in the stratified case, instead a number of integral constraints along the axis of rotation are derived allowing us to relate the interior motion to the surface forcing distributions. The unsteady low frequency waves with Tay...

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Simulation of equatorial and high-latitude jets on Jupiter in a deep convection model.

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Geophysical and astrophysical fluid dynamics beyond the traditional approximation

TL;DR: In this article, a review of the effects of abandoning the traditional approximation (TA) on geophysical fluid dynamics is presented, based on evidence from numerical and theoretical studies and laboratory and field experiments.
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Turbulent convection in rapidly rotating spherical shells: A model for equatorial and high latitude jets on Jupiter and Saturn

TL;DR: In this article, the authors show that deep convection in a spherical shell can generate zonal flow comparable to that observed on Jupiter and Saturn, including a broad prograde equatorial jet and multiple alternating jets at higher latitudes.
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A laboratory model for deep-seated jets on the gas giants

TL;DR: In this article, a laboratory study of turbulent flows reproduces the properties of jets in the atmospheres of gas giants, providing a better understanding of how these jets could extend deep into the planetary atmosphere.
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Deep two-dimensional turbulence: An idealized model for atmospheric jets of the giant outer planets

TL;DR: In this paper, the Taylor-Proudman theorem is applied to the dynamics of the global circulations of the Jovian atmospheres under the constraint of a deep configuration.
References
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Book

Geophysical Fluid Dynamics

TL;DR: In this article, the authors propose a quasigeostrophic motion of a Stratified Fluid on a Sphere (SFL) on a sphere, which is based on an Inviscid Shallow-Water Theory.
Journal ArticleDOI

Wind-Driven Currents in a Baroclinic Ocean; with Application to the Equatorial Currents of the Eastern Pacific

TL;DR: This analysis indicates that the inability of these exceptional adenine-dependent, methionine-independent cultures to produce the pink pigment was due to some mechanism which is restored to activity following hybridization.
Journal ArticleDOI

The Eigenfunctions of Laplace's Tidal Equations over a Sphere

TL;DR: In this paper, the eigenvalues of Laplace's tidal equations governing a thin layer of fluid on a rotating sphere, for a complete range of the parameter e ( omega = rate of rotation, R = radius, g = gravity, h = depth of fluid layer).
Journal ArticleDOI

Free Hydromagnetic Oscillations of the Earth's Core and the Theory of the Geomagnetic Secular Variation

TL;DR: In this article, free hydromagnetic oscillations of a rotating spherical shell of an incompressible fluid are investigated by means of a simple theoretical model for each spatial harmonic, rotation gives rise to two distinct modes of oscillation, "magnetic" and "inertial" which propagate with different velocities.
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