GSTDTAP  > 气候变化
DOI10.1029/2018GL078104
Hysteresis and Resilience of the AMOC in an Eddy-Permitting GCM
Jackson, L. C.; Wood, R. A.
2018-08-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2018
卷号45期号:16页码:8547-8556
文章类型Article
语种英语
国家England
英文摘要

We show a quasi-irreversible shutdown (hysteresis) of the Atlantic meridional overturning circulation (AMOC) in an unfluxadjusted global climate model with an eddy-permitting ocean. This global climate model is a prototype of one submitted to the sixth Coupled Model Intercomparison Project and is the most comprehensive model to show this behavior. The AMOC has a resilience timescale for a given hosing: If the hosing exceeds the critical hosing for collapse for only a limited time, the AMOC recovers when the hosing is stopped. Beyond the critical time, when the hosing stops the AMOC stays in a weak state with no recovery within 200 years. We show that simple, observable metrics such as AMOC strength and mixed layer depth can indicate whether this critical resilience time has passed and that the mechanism controlling the presence of recovery is a positive advective feedback.


Plain Language Summary The Atlantic meridional overturning circulation (AMOC) is an important part of our climate system, which keeps the North Atlantic relatively warm. It is predicted to weaken under climate change. The AMOC may have a tipping point beyond which recovery is difficult, hence showing quasi-irreversibility (hysteresis). Although hysteresis has been seen in simple models, it has been difficult to demonstrate in comprehensive global climate models. We use a comprehensive global climate model to examine the AMOC response to the addition of freshwater (hosing) in the North Atlantic, such as from melting glaciers. The freshening weakens the AMOC, and if the AMOC is weakened sufficiently it remains in a weak state even when the hosing is stopped. We also introduce and demonstrate the concept of a timescale of resilience: Although a particular hosing might shut down the AMOC if experienced for long enough, the AMOC can recover if the hosing is only experienced for a limited time. Indicators of whether the AMOC can recover are discussed, with implications for monitoring. Results also have relevance for the modeling and policy communities in providing results that can be used to understand the uncertainties around an AMOC shutdown.


英文关键词AMOC hysteresis temporary resilience climate
领域气候变化
收录类别SCI-E
WOS记录号WOS:000445612500074
WOS关键词MERIDIONAL OVERTURNING CIRCULATION ; THERMOHALINE CIRCULATION ; MULTIPLE EQUILIBRIA ; GLOBAL OCEAN ; NORTH-ATLANTIC ; CLIMATE ; STABILITY ; SEA ; FEEDBACKS ; RECOVERY
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/25750
专题气候变化
作者单位Met Off Hadley Ctr, Exeter, Devon, England
推荐引用方式
GB/T 7714
Jackson, L. C.,Wood, R. A.. Hysteresis and Resilience of the AMOC in an Eddy-Permitting GCM[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(16):8547-8556.
APA Jackson, L. C.,&Wood, R. A..(2018).Hysteresis and Resilience of the AMOC in an Eddy-Permitting GCM.GEOPHYSICAL RESEARCH LETTERS,45(16),8547-8556.
MLA Jackson, L. C.,et al."Hysteresis and Resilience of the AMOC in an Eddy-Permitting GCM".GEOPHYSICAL RESEARCH LETTERS 45.16(2018):8547-8556.
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