Why is the AMOC monostable in coupled general circulation models?

Journal of Climate

Volumn 27, Issue 6, 2014, Pages 2427-2443

  Liu, Wei ^a   Liu, Zhengyu ^a,b   Brady, Esther C ^c  

^a UNIVERSITY OF WISCONSIN MADISON   (United States)

^b PEKING UNIVERSITY   (China)

^c NATIONAL CENTER FOR ATMOSPHERIC RESEARCH   (United States)

Author keywords

Feedback; Meridional overturning circulation; Ocean circulation; Stability; Thermocline circulation

Indexed keywords

ATMOSPHERIC TURBULENCE; CLIMATE MODELS; CONVERGENCE OF NUMERICAL METHODS; EXPERIMENTS; FEEDBACK; TROPICS; WATER;

ATLANTIC MERIDIONAL OVERTURNING CIRCULATIONS; COMMUNITY CLIMATE SYSTEM MODEL; COUPLED GENERAL CIRCULATION MODELS; FRESHWATER TRANSPORTS; MERIDIONAL OVERTURNING CIRCULATIONS; OCEAN CIRCULATION; STABILITY INDICATORS; THERMOCLINE CIRCULATION;

OCEANOGRAPHY;

AIR-SEA INTERACTION; ATMOSPHERIC GENERAL CIRCULATION MODEL; OCEANIC CIRCULATION; OVERTURN; SALINITY; SEA SURFACE TEMPERATURE; THERMOCLINE;

ATLANTIC OCEAN; ATLANTIC OCEAN (SOUTH);

EID: 84896082741     PISSN: 08948755     EISSN: None     Source Type: Journal    
DOI: 10.1175/JCLI-D-13-00264.1     Document Type: Article

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