Labrador Sea Water

E196739

Labrador Sea Water is a cold, dense, and relatively fresh deep water mass formed by winter convection in the Labrador Sea that contributes significantly to the North Atlantic Deep Water and global ocean circulation.

All labels observed (1)

Label Occurrences
Labrador Sea Water canonical 4

How this entity was disambiguated

Statements (50)

Predicate Object
instanceOf deep water mass ⓘ
intermediate water mass ⓘ
water mass ⓘ
ageCharacteristic relatively young deep water compared to Antarctic Bottom Water ⓘ
associatedWith Labrador Sea deep convection events ⓘ
North Atlantic Oscillation variability ⓘ
basin Subpolar North Atlantic ⓘ
linked to: Nordic Seas
carbonCycleRole important sink for anthropogenic CO₂ ⓘ
circulationPathway spreads eastward into the Irminger Sea ⓘ
spreads into the Iceland Basin ⓘ
spreads southward along the western boundary of the North Atlantic ⓘ
climateRelevance indicator of variability in North Atlantic overturning ⓘ
sensitive to changes in surface heat and freshwater fluxes ⓘ
componentOf North Atlantic Deep Water ⓘ
contributesTo North Atlantic Deep Water ⓘ
densityClass σθ ≈ 27.7–27.8 kg/m³ ⓘ
depthRange intermediate to deep ocean ⓘ
~1000–2500 m ⓘ
formationMechanism brine rejection from sea-ice formation ⓘ
intense surface buoyancy loss ⓘ
surface cooling ⓘ
formationProcess deep convection ⓘ
winter convection ⓘ
formationSeason winter ⓘ
formedIn Labrador Sea ⓘ
influences distribution of tracers such as CFCs and nutrients in the deep North Atlantic ⓘ
storage of heat in the North Atlantic ⓘ
mixesWith Denmark Strait Overflow Water ⓘ
Iceland–Scotland Overflow Water ⓘ
Mediterranean Overflow Water ⓘ
monitoredBy Argo profiling floats ⓘ
linked to: Argo floats

hydrographic sections ⓘ
moored current meter arrays ⓘ
namedAfter Labrador Sea ⓘ
oceanRegion North Atlantic Ocean ⓘ
linked to: Atlantic Ocean
researchField physical oceanography ⓘ
roleInSystem important in global thermohaline circulation ⓘ
key component of Atlantic Meridional Overturning Circulation ⓘ
salinityCharacteristic fresher than underlying overflow waters ⓘ
salinityRange ~34.8–34.9 psu ⓘ
temperatureCharacteristic colder than overlying subtropical waters ⓘ
temperatureRange ~2–3 °C ⓘ
transportedBy Deep Western Boundary Current ⓘ
ventilationFunction transports oxygen to the deep ocean ⓘ
ventilates the deep North Atlantic ⓘ
waterMassCoreProperty distinct salinity minimum layer ⓘ
low potential vorticity core ⓘ
waterProperty cold ⓘ
dense ⓘ
relatively fresh ⓘ

How these facts were elicited

Referenced by (4)

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

Labrador Sea → hasWaterMass → Labrador Sea Water ⓘ
Irminger Basin → hasWaterMass → Labrador Sea Water ⓘ