North Atlantic Central Water

E733842

North Atlantic Central Water is a mid-depth water mass in the North Atlantic Ocean characterized by relatively uniform temperature and salinity, formed through the mixing of surface waters and influencing large-scale ocean circulation.

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Statements (30)

Predicate Object
instanceOf oceanographic feature
water mass
associatedWith North Atlantic subtropical gyre NERFINISHED
mode waters of the North Atlantic
basin North Atlantic Ocean NERFINISHED
circulationContext subtropical gyre of the North Atlantic
densityStructure weak vertical stratification within the layer
formationProcess mixing of surface waters
subduction of surface waters
hemisphere Northern Hemisphere NERFINISHED
influences North Atlantic gyre circulation
heat transport in the North Atlantic
large-scale ocean circulation
salt transport in the North Atlantic
isPartOf global thermocline water masses
liesAbove North Atlantic Intermediate Water NERFINISHED
liesBelow North Atlantic surface waters NERFINISHED
ocean Atlantic Ocean
propertyDistribution horizontally extensive layer of nearly uniform properties
relatedProcess ventilation of the thermocline
roleInClimate storage of heat in the upper ocean
storage of salt in the upper ocean
salinityCharacteristic relatively high salinity compared to overlying subpolar waters
scientificDiscipline physical oceanography
temperatureCharacteristic intermediate temperature between warm surface and colder deep waters
typicalDepthRange mid-depth
waterColumnProperty relatively uniform salinity
relatively uniform temperature
waterMassLayer thermocline layer
waterMassType central water

Referenced by (1)

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

Mediterranean Outflow Water mixesWith North Atlantic Central Water