The ocean circulation is driven by a combination of winds and surface buoyancy fluxes. We run a number of experiments with varied surface forcings and look at the spatial variations in ocean circulation on short and long time-scales.
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Geostrophic and thermal wind balance in FFM-CONTROL #57
Changing file name: TWR.ipynb to TWR_control.ipynb to be more descriptive of the FFM experiment being used in the notebook.