Linear theory of rotating fluids using spherical harmonics part I: Steady flows
From MaRDI portal
Publication:3773629
DOI10.1080/03091928708208811zbMath0634.76106OpenAlexW1983805589WikidataQ114640363 ScholiaQ114640363MaRDI QIDQ3773629
Publication date: 1987
Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1080/03091928708208811
spherical harmonicsrotating fluidsequatorial singularity of steady boundary layerssteady spin-up of a fluid
Related Items (7)
Convergence and round-off errors in a two-dimensional eigenvalue problem using spectral methods and Arnoldi-Chebyshev algorithm ⋮ Axisymmetric inertial modes in a spherical shell at low Ekman numbers ⋮ Stress-driven spin-down of a viscous fluid within a spherical shell ⋮ Inertial waves in a differentially rotating spherical shell ⋮ Viscous dissipation by tidally forced inertial modes in a rotating spherical shell ⋮ Internal shear layers in librating spherical shells: the case of periodic characteristic paths ⋮ Gravito-inertial waves in a differentially rotating spherical shell
Cites Work
- The almost-rigid rotation of viscous fluid between concentric spheres
- Quasi-steady flow of a rotating stratified fluid in a sphere
- Patterns of convection in spherical shells. Part 2
- On almost rigid rotations. Part 2
- On the lnviscid Theory of Rotating Fluids
- Spin-up of a strongly stratified fluid in a sphere
- Viscous incompressible flow between concentric rotating spheres. Part 1. Basic flow
- An equatorial boundary layer
This page was built for publication: Linear theory of rotating fluids using spherical harmonics part I: Steady flows