Fig. 8: Atmospheric circulation bias in climate model simulations.
From: Dominant inflation of the Arctic Ocean’s Beaufort Gyre in a warming climate

a Sea level pressure (SLP) in atmosphere reanalysis JRA55-do averaged over the period of 1960–2009. b CMIP6 multi-model mean (MMM) SLP averaged over the period of 1960–2009. c, SLP bias of CMIP6 MMM averaged over the period of 1960–2009. d, CMIP6 MMM SLP averaged over the period of 2081–2100. e Corrected (CRD) CMIP6 MMM SLP averaged over the period of 2081–2100. f–i, the same as (b–e), but for the SLP from the FIO-ESM2.1 simulation.