Working Up Hills: Dynamics over Sloping Topography with Bottom-Enhanced Diffusion
The deep ocean circulation is known to have influence even at the surface, through means such as the Meridional Overturning Circulation (MOC). Initial theories on abyssal circulation and mixing have been improving, based on observation of both physical and numerical experiments. By tracing this pr...
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| Language: | English |
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2012
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| Online Access: | https://doi.org/10.7916/D84Q820C |