Mechanisms of millennial-scale atmospheric CO 2 change in numerical model simulations

• Published in: Quaternary Science Reviews
• 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: unknown
• Published: Elsevier 2019
• Subjects: 13 Climate Action; 14 Life Below Water; anzsrc-for: 04 Earth Sciences; anzsrc-for: 21 History and Archaeology; Antarctic; Southern Ocean; Pacific; Antarc*; North Atlantic; Sea ice
• Online Access: http://hdl.handle.net/1959.4/unsworks_66924; https://doi.org/10.1016/j.quascirev.2019.05.013

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 varying export production, and changes in carbon storage in the Atlantic (rising), in other ocean basins (generally decreasing) and on land (more varied). Positive or negative CO2,atm changes are simulated during AMOC minima due to a spatially and temporally varying dominance of individual terrestrial and oceanic drivers (and compensating effects between them) across the different models. In contrast, AMOC recoveries are often accompanied by rising CO2,atm levels, which are mostly driven by ocean carbon release (albeit from different regions). The magnitude of simulated CO2,atm rise broadly scales with the duration of the AMOC perturbation (i.e., the stadial length). When freshwater is added to the Southern Ocean, reduced deep-ocean ventilation drives a CO2,atm drop via reduced carbon release from the Southern Ocean. Although the impacts of shifted southern-hemisphere westerlies are inconsistent across model simulations, their intensification raises CO2,atm via enhanced Southern Ocean Ekman pumping. Increased ...