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 |
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Number of pages | 9 |
Journal | Applicable Analysis |
DOIs | |
Publication status | Published - 4 Jun 2020 |
Keywords
- Geophysical flow
- boundary-value problem
- viscosity
- vorticity