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The response of an ocean with a single active dynamical layer (notionally with an infinitely thick upper layer above it, of slightly less density) to localized buoyancy forcing on a beta-plane is cons...
Abyssal Circulation in a Circumpolar Basin Driven by Discrete Sources of Buoyancy
Abyssal Circulation Discrete Sources Circumpolar Basin Driven
2008/12/3
The response of the deep ocean to periodic and steady forcing by mass sources is considered, in the presence of fluid loss, diffusion, and topography, which may or may not have regions of closed plane...