Regional asymmetries in ocean heat and carbon storage due to dynamic redistribution in climate model projections

• Published in: Journal of Climate
• Main Authors: Williams, Richard G., Katavouta, Anna, Roussenov, Vassil
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2021
• Subjects: Southern Ocean; North Atlantic
• Online Access: http://nora.nerc.ac.uk/id/eprint/531095/; https://nora.nerc.ac.uk/id/eprint/531095/1/%5B15200442%20-%20Journal%20of%20Climate%5D%20Regional%20Asymmetries%20in%20Ocean%20Heat%20and%20Carbon%20Storage%20due%20to%20Dynamic%20Redistribution%20in%20Climate%20Model%20Projections.pdf; https://doi.org/10.1175/JCLI-D-20-0519.1

Projected changes in ocean heat and carbon storage are assessed in terms of the added and redistributed tracer using a transport-based framework, which is applied to an idealized climate model and a suite of six CMIP5 Earth system models following an annual 1% rise in atmospheric CO2. Heat and carbon budgets for the added and redistributed tracer are used to explain opposing regional patterns in the storage of ocean heat and carbon anomalies, such as in the tropics and subpolar North Atlantic, and the relatively reduced storage within the Southern Ocean. Here the added tracer takes account of the net tracer source and the advection of the added tracer by the circulation, while the redistributed tracer takes account of the time-varying circulation advecting the preindustrial tracer distribution. The added heat and carbon often have a similar sign to each other with the net source usually acting to supply the tracer. In contrast, the redistributed heat and carbon consistently have an opposing sign to each other due to the opposing gradients in the preindustrial temperature and carbon. These different signs in heat and carbon redistribution can lead to regional asymmetries in the climate-driven changes in ocean heat and carbon storage. For a weakening in the Atlantic overturning and strengthening in the Southern Ocean residual circulation, the high latitudes are expected to have heat anomalies of variable sign and carbon anomalies of a consistently positive sign, since added and redistributed tracers are opposing in sign for heat and the same sign for carbon there.