Global Cooling Hiatus Driven by an AMOC Overshoot in a Carbon Dioxide Removal Scenario
Soon‐Il An, Jongsoo Shin, Sang‐Wook Yeh, Seok‐Woo Son, Jong‐Seong Kug, Seung‐Ki Min, Hyojeong Kim
Abstract
Abstract The reversibility of global mean surface temperature was examined by a transient CO 2 reversibility experiment using an Earth system model. The results showed that after CO 2 ramp‐up toward CO 2 quadrupling and ramp‐down returned to the present‐day level, the global mean surface temperature kept decreasing but stopped to change for ∼40 years in the early net‐zero CO 2 emission period. This period, referred to a cooling hiatus, resulted from a compensation between Southern Hemisphere cooling and Northern Hemisphere warming. The Northern Hemisphere warming was centered over the North Atlantic. This localized warming was caused by an excessive heat advection by a delayed and surpassed Atlantic Meridional Overturning Circulation (AMOC) to CO 2 forcing. During the progression of CO 2 change, the meridional salinity gradient between subtropic and subpolar regions was enhanced, and the oceanic stratification in subpolar North Atlantic was reduced due to accumulated heat and reduced vertical salt import in the deeper ocean. As AMOC started to recover, consequently, the enhanced salt advection feedback and the relaxed buoyant force resulted in AMOC overshoot.