Abstract
We discuss a mathematical model for the equatorial current across the Pacific Ocean, obtained as a leading-order solution to the Navier-Stokes governing equations for geophysical flows in a rotating frame.
| Original language | English |
|---|---|
| Pages (from-to) | 1147-1155 |
| Number of pages | 9 |
| Journal | Applicable Analysis |
| Volume | 101 (2022) |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - 4 Jun 2020 |
Keywords
- Geophysical flow
- boundary-value problem
- viscosity
- vorticity