Extended Data Fig. 5: Deep ocean carbon accumulation and meridional overturning rates in eight CMIP6 models under the SSP1-2.6 warming scenario.
From: Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation
The time series of DIC partitioning in CanESM5 (A), GFDL-ESM4 (B), IPSL-CM6A-LR (C), MPI-ESM1-2-HR (D), MPI-ESM1-2-LR (E), CanESM5-CanOE (F), CNRM-ESM2-1 (G) and UKESM1-0-LL (H), where the black, red and blue lines represent the total DIC, regenerated DIC and preformed DIC below 2000m depth (PgC/yr). Changing rates of the Southern-sourced Meridional Overturning Circulation (SMOC) and the Atlantic Meridional Overturning Circulation (AMOC) are also shown for each model.
