Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations ...

• Main Authors: Gottschalk, J, Battaglia, G, Fischer, H, Frölicher, TL, Jaccard, SL, Jeltsch-Thömmes, A, Joos, F, Köhler, P, Meissner, KJ, Menviel, L, Nehrbass-Ahles, C, Schmitt, J, Schmittner, A, Skinner, LC, Stocker, TF
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2019
• Subjects: Palaeoclimate modelling; Carbon cycle; Atmospheric CO2 variations; Freshwater hosing; Southern-hemisphere westerlies; Sea ice; Dust; Antarctic; Pacific; Southern Ocean; Antarc*; North Atlantic
• Online Access: https://dx.doi.org/10.17863/cam.46168; https://www.repository.cam.ac.uk/handle/1810/299106

Numerical models are important tools for understanding the processes and feedbacks in the Earth system, including those involving changes in atmospheric CO2 (CO2,atm) concentrations. Here, we compile 55 published model studies (consisting of 778 individual simulations) that assess the impact of six forcing mechanisms on millennial-scale CO2,atm variations: changes in freshwater supply to the North Atlantic and Southern Ocean, the strength and position of the southern-hemisphere westerlies, Antarctic sea ice extent, and aeolian dust fluxes. We generally find agreement on the direction of simulated CO2,atm change across simulations, but the amplitude of change is inconsistent, primarily due to the different complexities of the model representation of Earth system processes. When freshwater is added to the North Atlantic, a reduced Atlantic Meridional Overturning Circulation (AMOC) is generally accompanied by an increase in Southern Ocean- and Pacific overturning, reduced Antarctic sea ice extent, spatially ...