Explicit two-dimensional solutions for the ocean flow in arctic gyres
From MaRDI portal
Publication:2003532
DOI10.1007/s00605-018-1198-3zbMath1420.35425OpenAlexW2807021817MaRDI QIDQ2003532
Publication date: 9 July 2019
Published in: Monatshefte für Mathematik (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1007/s00605-018-1198-3
Hydrology, hydrography, oceanography (86A05) General theory of rotating fluids (76U05) Linear boundary value problems for ordinary differential equations (34B05) PDEs in connection with geophysics (35Q86)
Related Items (5)
Existence and stability results for a second-order differential equation for the Antarctic circumpolar current ⋮ Nagumo-type uniqueness and stability for nonlinear differential equations on semi-infinite intervals ⋮ Study on a second-order ordinary differential equation for the ocean flow in arctic gyres ⋮ Multiple solutions for an elliptic equation from the antarctic circumpolar current ⋮ Study of an elliptic partial differential equation modeling the ocean flow in arctic gyres
Cites Work
- Unnamed Item
- Unnamed Item
- Monotone solutions of a nonlinear differential equation for geophysical fluid flows
- A nonlinear two-point boundary-value problem in geophysics
- On a differential equation arising in geophysics
- A steady, purely azimuthal flow model for the antarctic circumpolar current
- A weighted Sturm-Liouville problem related to Ocean flows
- Global bifurcation of steady gravity water waves with critical layers
- Large Amplitude Steady Periodic Waves for Fixed-Depth Rotational Flows
- Nonlinear Water Waves with Applications to Wave-Current Interactions and Tsunamis
- On a nonlinear integral equation for the ocean flow in arctic gyres
- Large gyres as a shallow-water asymptotic solution of Euler’s equation in spherical coordinates
- The Mercator and Stereographic Projections, and Many in Between
- The dynamics of waves interacting with the Equatorial Undercurrent
This page was built for publication: Explicit two-dimensional solutions for the ocean flow in arctic gyres