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 Ocean ⓘ
linked to: South Atlantic

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 North Atlantic Ocean ⓘ
linked to: 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.