Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8886556 | Ocean Modelling | 2017 | 4 Pages |
Abstract
We demonstrate a simple method to quickly spin up (equilibrate) the temperature field of a turbulent idealised primitive equation ocean gyre model. We make use of the assumption that both velocity fields and non-linear eddy advection terms equilibrate on a shorter timescale than tracer fields.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
Fenwick C. Cooper,