The stability of an evolving Atlantic meridional overturning circulation

In this study, we propose a generalized stability indicator, L, for a slowly evolving and quasi-steady Atlantic meridional overturning circulation (AMOC), which represents a feedback related to the AMOC and its associated freshwater transport within the Atlantic basin. As an improvement from previou...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Liu, Wei, Liu, Zhengyu, Hu, Aixue
Other Authors: Liu, W (reprint author), Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Key Lab Meteorol Disaster, Minist Educ, Nanjing, Jiangsu, Peoples R China., Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Key Lab Meteorol Disaster, Minist Educ, Nanjing, Jiangsu, Peoples R China., Univ Wisconsin, Ctr Climat Res, Madison, WI USA., Peking Univ, Lab Climate Ocean & Atmosphere Studies, Beijing 100871, Peoples R China., Natl Ctr Atmospher Res, Climate & Global Dynam Div, Boulder, CO 80307 USA.
Format: Journal/Newspaper
Language:English
Published: geophysical research letters 2013
Subjects:
AMOC stability
AMOC hysteresis
feedback
MULTIPLE EQUILIBRIA REGIME
MIXED BOUNDARY-CONDITIONS
THERMOHALINE CIRCULATION
OCEAN CIRCULATION
BERING STRAIT
CLIMATE
MODEL
CCSM3
INSTABILITY
HYSTERESIS
Arctic
Bering Strait
Climate change
North Atlantic
Online Access:https://hdl.handle.net/20.500.11897/225138
https://doi.org/10.1002/grl.50365
Description
Summary:In this study, we propose a generalized stability indicator, L, for a slowly evolving and quasi-steady Atlantic meridional overturning circulation (AMOC), which represents a feedback related to the AMOC and its associated freshwater transport within the Atlantic basin. As an improvement from previous indicators for the AMOC in equilibrium, this generalized indicator does not require a divergence-free freshwater transport in the Atlantic for a collapsed AMOC, which enables it to correctly monitor the AMOC stability through the AMOC hysteresis loop in the coupled atmosphere-ocean general circulation models. From the simulation, the indicator L suggests that the AMOC is in a stable regime, with single equilibrium under the present-day and the Last Glacial Maximum (LGM) climates. However, under the present-day climate, a Bering Strait (BS) closure will diminish the freshwater outflow from the North Atlantic into the Arctic as the AMOC collapses, resulting in a freshwater convergence in the Atlantic basin and making the AMOC reside in a stable collapsed state, i.e., the AMOC exhibits characteristics of multiple equilibria. Further analysis shows that the BS effect is much reduced under the LGM climate. This generalized indicator L has great implications for paleoclimate studies in understanding the abrupt climate change due to the instability of the AMOC. Geosciences, Multidisciplinary SCI(E) EI 6 ARTICLE 8 1562-1568 40

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