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Focusing on the lower-tier of climate models that require less computational strength and simplicity without explicitly resolving atmospheric and oceanic fluid dynamics, the main approach over the last year and a half was to represent nonlinear processes through linearised parameterisations for diffusive horizontal and vertical exchange processes between the interfaces, and to implement the ocean component of the model coupled to the single atmospheric slab via sensible and latent heat fluxes represented as aerodynamic bulk fluxes

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