Free-surface, purely azimuthal equatorial flows in spherical coordinates with stratification
DOI10.1016/j.jde.2018.11.017zbMath1412.35241OpenAlexW2901158435WikidataQ128887283 ScholiaQ128887283MaRDI QIDQ1731868
David Henry, Calin Iulian Martin
Publication date: 14 March 2019
Published in: Journal of Differential Equations (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.jde.2018.11.017
Coriolis forceimplicit function theoremspherical coordinatesazimuthal flowsvariable (linear) densityshort-wavelength perturbation
PDEs in connection with fluid mechanics (35Q35) Hydrology, hydrography, oceanography (86A05) General theory of rotating fluids (76U05) Free boundary problems for PDEs (35R35) Stability and instability of geophysical and astrophysical flows (76E20) PDEs in connection with geophysics (35Q86) Euler equations (35Q31)
Related Items (26)
Cites Work
- Instability of equatorially trapped waves in stratified water
- An exact solution for equatorial geophysical water waves with an underlying current
- Local stability for an exact steady purely azimuthal flow which models the antarctic circumpolar current
- Free-surface capillary-gravity azimuthal equatorial flows
- Exact, purely azimuthal stratified equatorial flows in cylindrical coordinates
- Local stability for an exact steady purely azimuthal equatorial flow
- Instability of internal equatorial water waves
- Instability of equatorial water waves with an underlying current
- An exact solution for equatorial waves
- Local stability conditions in fluid dynamics
- Instability criteria for the flow of an inviscid incompressible fluid
- On three-dimensional Gerstner-like equatorial water waves
- On the short-wavelength stabilities of some geophysical flows
- Application of the ideas and techniques of classical fluid mechanics to some problems in physical oceanography
- Large gyres as a shallow-water asymptotic solution of Euler’s equation in spherical coordinates
- Equatorially trapped nonlinear water waves in a -plane approximation with centripetal forces
- On the existence of free-surface azimuthal equatorial flows
- Gerstner waves in the presence of mean currents and rotation
- An Explicit Solution for Deep Water Waves With Coriolis Effects
- The dynamics of waves interacting with the Equatorial Undercurrent
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