Response of Southern Ocean convection and abbyssal overturning to surface buoyancy perturbations.
This study explores how buoyancy-driven modulations in the abyssal overturning circulation affect Southern Ocean temperature and salinity in an eddy-permitting ocean model. Consistent with previous studies, the modeled surface ocean south of 50°S cools and freshens in response to enhanced surface freshwater fluxes. Paradoxically, upper-ocean cooling also occurs for small increases in the surface relaxation temperature. In both cases, the surface cooling and freshening trends are linked to...[Show more]
|Collections||ANU Research Publications|
|Source:||Journal of Climate|
|01_Morrison_Response_of_Southern_Ocean_2015.pdf||2.07 MB||Adobe PDF||Request a copy|
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