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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Increasing both heat flux and wind stress by a certain factor #42
In these set of experiment, we increase both heat flux and wind stress by a certain factor (1.5x each to begin with). We run these simulations for 100 years and observe the resulting changes in ocean circulation.
In these set of experiment, we increase both heat flux and wind stress by a certain factor (1.5x each to begin with). We run these simulations for 100 years and observe the resulting changes in ocean circulation.