Response of atmospheric pCO2 to a strong AMOC weakening under low and high emission scenarios

• Published in: Climate dynamics Vol. 62; no. 8; pp. 7559 - 7574
• Main Authors: Boot, Amber A., von der Heydt, Anna S., Dijkstra, Henk A.
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.08.2024; Springer Nature B.V
• Subjects: Anthropogenic factors; Atlantic Meridional Overturning Circulation (AMOC); Carbon; Carbon cycle; Climate; Climate system; Climatology; Earth; Earth and Environmental Science; Earth Sciences; Emissions; Freshwater; Geophysics/Geodesy; Greenhouse effect; Greenhouse gases; Human influences; Inland water environment; Oceanography; Original Article; risk; uncertainty; Carbon cycle; AMOC weakening; Climate change; Marine biosphere; Atmospheric pCO; Atlantic meridional overturning circulation
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-024-07295-y

The Earth System is warming due to anthropogenic greenhouse gas emissions which increases the risk of passing a tipping point in the Earth System, such as a collapse of the Atlantic Meridional Overturning Circulation (AMOC). An AMOC weakening can have large climate impacts which influences the marine and terrestrial carbon cycle and hence atmospheric pCO 2 . However, the sign and mechanism of this response are subject to uncertainty. Here, we use a state-of-the-art Earth System Model, the Community Earth System Model v2 (CESM2), to study the atmospheric pCO 2 response to an AMOC weakening under low (SSP1-2.6) and high (SSP5-8.5) emission scenarios over the years 2015–2100. A freshwater flux anomaly in the North Atlantic strongly weakens the AMOC, and we simulate a weak positive pCO 2 response of 0.45 and 1.3 ppm increase per AMOC decrease in Sv for SSP1-2.6 and SSP5-8.5, respectively. For SSP1-2.6 this response is driven by both the oceanic and terrestrial carbon cycles, whereas in SSP5-8.5 it is solely the ocean that drives the response. However, the spatial patterns of both the climate and carbon cycle response are similar in both emission scenarios over the course of the simulation period (2015–2100), showing that the response pattern is not dependent on cumulative CO 2 emissions up to 2100. Though the global atmospheric pCO 2 response might be small, locally large changes in both the carbon cycle and the climate system occur due to the AMOC weakening, which can have large detrimental effects on ecosystems and society.