Dominance of the Southern Ocean in Anthropogenic Carbon and Heat Uptake in CMIP5 Models

The authors assess the uptake, transport, and storage of oceanic anthropogenic carbon and heat over the period1861‐2005inanewset ofcoupledcarbon‐climateEarthsystemmodelsconductedforthefifthphaseof the Coupled Model Intercomparison Project (CMIP5), with a particular focus on the Southern Ocean. Simulations show that the Southern Ocean south of 308S, occupying 30% of global surface ocean area, accounts for 43%63% (4265PgC) of anthropogenic CO2and 75%622% (2369 310 22 J) of heat uptake by the ocean over the historical period. Northward transport out of the Southern Ocean is vigorous, reducing the storage to 33 6 6Pg anthropogenic carbon and 12 6 7 3 10 22 J heat in the region. The CMIP5 models, as a class, tend to underestimate the observation-based global anthropogenic carbon storage but simulate trends inglobaloceanheatstorageoverthelast50yearswithinuncertaintiesofobservation-basedestimates.CMIP5 models suggest global and Southern Ocean CO2 uptake have been largely unaffected by recent climate variability and change. Anthropogenic carbon and heat storage show a common broad-scale pattern of change, but ocean heat storage is more structured than ocean carbon storage. The results highlight the significance of the Southern Ocean for the global climate and as the region where models differ the most in representation of anthropogenic CO2 and, in particular, heat uptake.