| Summary: | Thesis (Ph.D.)--University of Washington, 2024 This dissertation investigates the role of ocean basin geometry in the circulation of the ocean, of the atmosphere, and in shaping the global climate system as a whole. To explore this topic, a major component of this dissertation is the development of a novel coupled climate model with configurable bathymetry, orography, and coastline geometry. Here I developed an ocean--atmosphere--sea-ice model that allows the testing of different theories for the development of major hemispheric asymmetries in the climate system. The model can be configured with a wide range of continental configurations. When configured with two ocean basins -- one that is narrow and Atlantic-like and one wide and Pacific-like -- and forced with zonally uniform atmospheric conditions in an ocean-only setup, the pole-to-pole, cross-equatorial meridional overturning circulation (MOC) and associated northern high latitude deep water formation localizes to the narrower of two ocean basins. This is similar to the ocean circulation in the real world, characterized by an Atlantic meridional overturning circulation (AMOC) and neither deep water formation nor cross equatorial overturning circulation in the Pacific. Widening the narrow basin increases the strength of the overturning circulation, in contrast to previous idealized geometry ocean-only studies. Also, the shape with which the basin widens matters for the magnitude and pattern by which the MOC strengthens. For instance, maintaining straight, meridional coastlines and widening the ocean basins results in different changes to ocean circulation than widening the ocean basin by creating slanted coastlines. I show that adding an atmosphere and a land model to form a fully-coupled model reveals vastly different results. Coupling the ocean--sea-ice model to an atmosphere--land model yields a surprising result of cross-equatorial MOC and northern deep water formation in the wide basin. MOC occurs in the wide basin, where negative surface buoyancy ...
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