Oceanic hindcast simulations at high resolution suggest that the Atlantic MOC is bistable

Geophysical Research Letters

Volumn 40, Issue 12, 2013, Pages 3069-3073

  Deshayes, J ^a   Treguier A M ^b   Barnier, B ^c   Lecointre, A ^d   Sommer, J Le ^c   Molines, J M ^c   Penduff, T ^c   Bourdalle Badie R ^e   Drillet, Y ^e   Garric, G ^e   Benshila, R ^f   Madec, G ^f   Biastoch, A ^g   Boning C W ^g   Scheinert, M ^g   Coward, A C ^h   Hirschi, J J M ^h  

^a UNIVERSITY OF CAPE TOWN   (South Africa)

^b LPO   (France)

^c OBSERVATOIRE DE GRENOBLE   (France)

^d LEGI   (France)

^e MERCATOR OCÉAN   (France)

^f UNIVERSITÉ PIERRE ET MARIE CURIE   (France)

^g GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^h NOC   (United Kingdom)

Author keywords

AMOC; bistability; freshwater; modeling

Indexed keywords

AMOC; ATLANTIC MERIDIONAL OVERTURNING CIRCULATIONS; CLIMATE SCENARIOS; DEEP-WATER FORMATION; FRESHWATER; FRESHWATER TRANSPORTS; HIGH RESOLUTION; SOUTH ATLANTIC;

CLIMATE MODELS; INTERNATIONAL TRADE; MODELS; OPTICAL BISTABILITY; WATER;

OCEANOGRAPHY;

ADVECTION; CLIMATE MODELING; DEEP WATER FORMATION; FRESHWATER INPUT; HINDCASTING; MARINE ATMOSPHERE; MERIDIONAL CIRCULATION; OVERTURN;

ATLANTIC OCEAN; ATLANTIC OCEAN (NORTH); ATLANTIC OCEAN (SOUTH);

EID: 84880532654     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1002/grl.50534     Document Type: Article

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