Article ID Journal Published Year Pages File Type
8886556 Ocean Modelling 2017 4 Pages PDF
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
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