Global Cooling Hiatus Driven by an AMOC Overshoot in a Carbon Dioxide Removal Scenario

Abstract The reversibility of global mean surface temperature was examined by a transient CO2 reversibility experiment using an Earth system model. The results showed that after CO2 ramp‐up toward CO2 quadrupling and ramp‐down returned to the present‐day level, the global mean surface temperature ke...

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Bibliographic Details
Published in:Earth's Future
Main Authors: Soon‐Il An, Jongsoo Shin, Sang‐Wook Yeh, Seok‐Woo Son, Jong‐Seong Kug, Seung‐Ki Min, Hyo‐Jeong Kim
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2021
Subjects:
AMOC overshoot
delay AMOC response
global cooling hiatus
net‐zero CO2 emission
oceanic stratification
salt advection feedback
Environmental sciences
GE1-350
Ecology
QH540-549.5
North Atlantic
Online Access:https://doi.org/10.1029/2021EF002165
https://doaj.org/article/c1c17cdde8a24c9e98f2458a7e9fdd27
Description
Summary:Abstract The reversibility of global mean surface temperature was examined by a transient CO2 reversibility experiment using an Earth system model. The results showed that after CO2 ramp‐up toward CO2 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 CO2 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 CO2 forcing. During the progression of CO2 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.

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