A boundary-value problem arising in the modelling of equatorial wind-drift currents
DOI10.1007/S00605-021-01552-6zbMATH Open1490.35338OpenAlexW3141809153MaRDI QIDQ2117276
Publication date: 21 March 2022
Published in: Monatshefte für Mathematik (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1007/s00605-021-01552-6
PDEs in connection with fluid mechanics (35Q35) Hydrology, hydrography, oceanography (86A05) Meteorology and atmospheric physics (86A10) Existence problems for PDEs: global existence, local existence, non-existence (35A01) PDEs in connection with geophysics (35Q86) Uniqueness problems for PDEs: global uniqueness, local uniqueness, non-uniqueness (35A02) Geophysical flows (76U60)
Cites Work
- Global bifurcation of steady gravity water waves with critical layers
- A hyperbolic-type azimuthal velocity model for equatorial currents
- The modeling of the equatorial undercurrent using the Navier–Stokes equations in rotating spherical coordinates
- Frictional effects in wind-driven ocean currents
- Dynamics of the thermocline in the equatorial region of the Pacific ocean
- On the existence of free-surface azimuthal equatorial flows
- The dynamics of waves interacting with the Equatorial Undercurrent
- Equatorial wave-current interactions
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