Transient overturning compensation between Atlantic and Indo-Pacific basins
[MOC streamfunction averaged between 2006-2015 (top) and its changes from 2006-2015 to 2090-2100 (bottom), simulated by CESM.]
Climate models consistently project (i) a decline in the formation of North Atlantic Deep Water (NADW) and (ii) a strengthening of the Southern Hemisphere westerly winds in response to anthropogenic greenhouse gas forcing. These two processes suggest potentially conflicting tendencies of the Atlantic Meridional Overturning Circulation (AMOC): a weakening AMOC due to changes in the North Atlantic but a strengthening AMOC due to changes in the Southern Ocean (see figure above).
We propose that the adjustment of the Indo-Pacific overturning circulation is a critical component in mediating AMOC changes. Using a hierarchy of ocean and climate models, we show that the Indo-Pacific overturning circulation provides the first response to AMOC changes through wave processes, whereas the Southern Ocean overturning circulation responds on longer (centennial to millenial) timescales that are determined by eddy diffusion processes. Changes in the Indo-Pacific overturning circulation compensate AMOC changes, which allows the Southern Ocean overturning circulation to evolve independently of the AMOC, at least over timescales up to many decades. In a warming climate, the Indo-Pacific develops an overturning circulation anomaly associated with the weakening AMOC that is characterized by a northward transport close to the surface and a southward transport in the deep ocean, which could effectively redistribute heat between the basins. Our results highlight the importance of inter-basin exchange in the response of the global ocean overturning circulation to a changing climate.
What sets the AMOC depth?
Paleoclimate proxy data suggest that the AMOC was shallower at the Last Glacial Maximum than its preindustrial depth. Previous studies emphasized the Southern Ocean surface buoyancy forcing in setting the AMOC depth. Using a combination of model simulations and conceptual theories, we show that the dipyacnal processes, ignored in previous studies, could diminish the influece of Southern Ocean surface buoyancy forcing on the AMOC depth. A new schematic based on surface buoyancy distributions in both the Southern Ocean and the North Atlantic is proposed.
Deep Ocean Stratification
Previous studies have suggested that the global ocean density stratification below ∼3000 m is approximately set by its direct connection to the Southern Ocean surface density, which in turn is constrained by the atmosphere. Here the role of Southern Ocean surface forcing in glacial-interglacial stratification changes is investigated using a comprehensive climate model and an idealized conceptual model. Southern Ocean surface forcing is found to control the global deep ocean stratification up to ∼2000 m, which is much shallower than previously thought and contrary to the expectation that the North Atlantic surface forcing should strongly influence the ocean at intermediate depths. We show that this is due to the approximately fixed surface freshwater fluxes, rather than a fixed surface density distribution in the Southern Ocean as was previously assumed. These results suggest that Southern Ocean surface freshwater forcing controls glacial-interglacial stratification changes in much of the deep ocean.
Ref: Sun et al. (2016)
Coming soon …