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A coupled atmosphere-ocean model of thermohaline circulation, including wind-driven gyre circulation with an analytical solution

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Academic year: 2021

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Figure  1:  Diagram  of Stommel  (1961)  model.  Direction  of flow, q, shown is for salinity driven  circulation.
Figure 3: Shaffer  and Olsen  (2001) model:  atmospheric, surface, and deep ocean boxes
Table  1: Parameter Values  and Definitions
Figure 5:  Plot of meridional salinity difference  vs.  wind-forcing parameter, with m=n=1.
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