NADW

E140798

NADW is a cold, dense water mass formed in the North Atlantic that sinks and flows southward, playing a key role in the global ocean circulation and climate system.

All labels observed (1)

Label Occurrences
NADW canonical 1

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf deep water mass
water mass
affects distribution of dissolved oxygen in deep Atlantic
uptake of anthropogenic CO2
ageCharacteristic relatively young deep water
associatedWith Arctic sea ice conditions
North Atlantic Oscillation
climateRelevance indicator of AMOC strength
componentOf Atlantic Meridional Overturning Circulation
global thermohaline circulation
contrastsWith Antarctic Bottom Water
densityDriver high salinity
low temperature
flowsDirection southward
flowsInto South Atlantic
surface form: South Atlantic Ocean

Southern Ocean
formationProcess deep convection
thermohaline circulation
formationRegion Greenland Sea
Labrador Sea
Nordic Seas
formsIn overflows across Greenland–Scotland Ridge
subpolar North Atlantic
fullName North Atlantic Deep Water
influences North Atlantic climate
global climate system
sea level patterns
linkedTo glacial–interglacial climate changes
oceanBasin Atlantic Ocean
surface form: North Atlantic Ocean
partOfLayering lies above Antarctic Bottom Water
lies below Antarctic Intermediate Water
relativeDepth deep
roleInSystem carbon storage
heat transport
nutrient transport
salinityRange ~34.8–35.0 PSU
studiedIn physical oceanography
temperatureRange ~2–4 °C
timeScaleOfChange decadal to centennial variability
tracedBy CFC concentrations
nutrient concentrations
radiocarbon
typicalDepthRange 1500–4000 m
ventilationTimescale centuries
waterMassType intermediate-to-deep water
waterProperty cold
high density
high salinity

How these facts were elicited

Referenced by (1)

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