Atlantic Meridional Overturning Circulation

E4621

The Atlantic Meridional Overturning Circulation is a large-scale system of ocean currents that transports heat and salt through the Atlantic, strongly influencing regional and global climate.

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All labels observed (8)

Statements (64)

Predicate Object
instanceOf climate system component
ocean circulation system
thermohaline circulation component
abbreviation Atlantic Meridional Overturning Circulation self-linksurface differs
surface form: AMOC
affects Atlantic hurricane activity
carbon uptake by the ocean
precipitation patterns
sea level in the North Atlantic
sea surface temperature patterns
canExhibit abrupt changes
collapse in climate model simulations
multiple stable states
characterizedBy northward flow of warm surface waters
southward flow of cold deep waters
drivenBy freshwater fluxes
salinity gradients
surface heat fluxes
temperature gradients
wind forcing
hasComponent Deep Western Boundary Current
Gulf Stream
Gulf Stream
surface form: North Atlantic Current
hasProcess convection in the Labrador Sea
convection in the Nordic Seas
deep water formation in the North Atlantic
sinking of dense water masses
upwelling of deep waters
includesWaterMass Antarctic Bottom Water
North Atlantic Deep Water
influences Arctic climate
European climate
North Atlantic climate
global climate
regional climate
tropical Atlantic climate
linkedTo Dansgaard–Oeschger events in paleoclimate records
Heinrich events in paleoclimate records
locatedIn Atlantic Ocean
measuredIn Sverdrups
monitoredAt 26.5°N RAPID array
OSNAP array in the subpolar North Atlantic
monitoredBy moored instrument arrays
ocean reanalysis products
satellite observations
partOf Earth climate system
global overturning circulation
representedIn Earth system models
coupled climate models
risk large regional climate impacts if collapse occurs
potential weakening during the 21st century
sensitiveTo Arctic sea ice melt
Greenland Ice Sheet meltwater
anthropogenic climate change
changes in surface salinity
changes in surface temperature
studiedBy climate scientists
physical oceanographers
timescale centennial variability
decadal variability
multidecadal variability
transports heat
salt
typicalStrength about 15 to 20 Sverdrups at 26.5°N
uncertainty future evolution under greenhouse gas forcing

Referenced by (41)

Full triples — surface form annotated when it differs from this entity's canonical label.

Gulf Stream partOf Atlantic Meridional Overturning Circulation
Atlantic Meridional Overturning Circulation abbreviation Atlantic Meridional Overturning Circulation self-linksurface differs
this entity surface form: AMOC
Florida Current isComponentOf Atlantic Meridional Overturning Circulation
Newfoundland and Labrador shelf influences Atlantic Meridional Overturning Circulation
this entity surface form: North Atlantic ocean circulation
Denmark Strait featureOf Atlantic Meridional Overturning Circulation
North Atlantic Deep Water drivingForce Atlantic Meridional Overturning Circulation
Deep Western Boundary Current partOf Atlantic Meridional Overturning Circulation
South Atlantic subtropical gyre relatedTo Atlantic Meridional Overturning Circulation
Agulhas Current contributesTo Atlantic Meridional Overturning Circulation
Atlantic Ocean proper by Martha's Vineyard hasClimateInfluence Atlantic Meridional Overturning Circulation
this entity surface form: North Atlantic Ocean circulation
Loop Current contributesTo Atlantic Meridional Overturning Circulation
Antilles Current partOf Atlantic Meridional Overturning Circulation
Greenland Basin playsRoleIn Atlantic Meridional Overturning Circulation
Beaufort Gyre influences Atlantic Meridional Overturning Circulation
East Greenland Current componentOf Atlantic Meridional Overturning Circulation
West Spitsbergen Current componentOf Atlantic Meridional Overturning Circulation
8.2 kiloyear event relatedTo Atlantic Meridional Overturning Circulation
Tagus River estuary influencedBy Atlantic Meridional Overturning Circulation
this entity surface form: Atlantic Ocean currents
Greenland Sea gyre partOf Atlantic Meridional Overturning Circulation
this entity surface form: North Atlantic thermohaline circulation
Atlantic Water isPartOf Atlantic Meridional Overturning Circulation
Bjerknes compensation relatedTo Atlantic Meridional Overturning Circulation
Weddell Gyre influences Atlantic Meridional Overturning Circulation
Irminger Current partOf Atlantic Meridional Overturning Circulation
NADW componentOf Atlantic Meridional Overturning Circulation
South Atlantic Current partOf Atlantic Meridional Overturning Circulation
South Atlantic hasMajorCurrent Atlantic Meridional Overturning Circulation
Nordic Seas playsRoleIn Atlantic Meridional Overturning Circulation
Irminger Sea roleIn Atlantic Meridional Overturning Circulation
eastern Atlantic Ocean importantFor Atlantic Meridional Overturning Circulation
this entity surface form: North Atlantic thermohaline circulation
Mediterranean Outflow Water contributesTo Atlantic Meridional Overturning Circulation
this entity surface form: Atlantic meridional overturning circulation
Agulhas Retroflection influences Atlantic Meridional Overturning Circulation
Southwest Atlantic circulation system contributesTo Atlantic Meridional Overturning Circulation
Indian Ocean circulation connectedTo Atlantic Meridional Overturning Circulation
this entity surface form: Atlantic Ocean circulation via Agulhas leakage
equatorial Atlantic Ocean influences Atlantic Meridional Overturning Circulation
tropical Atlantic Ocean influences Atlantic Meridional Overturning Circulation
Greenland Ice Sheet (North American sector) affects Atlantic Meridional Overturning Circulation
Arctic Intermediate Water associatedWith Atlantic Meridional Overturning Circulation
Denmark Strait overflow pathway partOf Atlantic Meridional Overturning Circulation
Yucatán Channel influences Atlantic Meridional Overturning Circulation
North Atlantic subpolar gyre system partOf Atlantic Meridional Overturning Circulation
Arctic sea ice system interactsWith Atlantic Meridional Overturning Circulation