Irminger Basin

E643816

The Irminger Basin is a deep oceanic basin in the North Atlantic, lying beneath the Irminger Sea between Greenland and Iceland and forming part of the complex subpolar gyre system.

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Statements (45)

Predicate Object
instanceOf oceanic basin
submarine basin
approximateLatitudeRange about 58°N to 65°N
approximateLongitudeRange about 30°W to 45°W
basinType deep abyssal basin
boundedBy Iceland–Faroe Ridge region NERFINISHED
Reykjanes Ridge NERFINISHED
southeast Greenland continental margin
circulationInfluencedBy East Greenland Current NERFINISHED
Irminger Current NERFINISHED
circulationType cyclonic subpolar gyre circulation
connectedTo Iceland Basin NERFINISHED
Labrador Sea NERFINISHED
countryExclusiveEconomicZones Greenland NERFINISHED
Iceland NERFINISHED
floorComposition oceanic crust
hasFeature thick sedimentary cover in deeper parts
hasObservationNetwork oceanographic moorings and repeat hydrographic sections
hasOverflowPathway Denmark Strait overflow into deep North Atlantic
hasProcess deep convection in some winters
hasWaterMass Denmark Strait Overflow Water NERFINISHED
Irminger Sea Intermediate Water NERFINISHED
Labrador Sea Water NERFINISHED
importantFor deep water formation in the North Atlantic
ventilation of the subpolar gyre
isPartOf Greenland–Iceland–Norwegian Seas–North Atlantic system NERFINISHED
locatedIn North Atlantic Ocean NERFINISHED
locatedSoutheastOf Greenland NERFINISHED
locatedUnder Irminger Sea NERFINISHED
locatedWestOf Iceland NERFINISHED
maximumDepth approximately 3000–3500 m
namedAfter Carl Ludvig Christian Irminger NERFINISHED
near Denmark Strait NERFINISHED
oceanRegion Labrador–Irminger Seas region NERFINISHED
partOf Atlantic Meridional Overturning Circulation NERFINISHED
North Atlantic subpolar gyre NERFINISHED
subpolar North Atlantic
roleInClimate carbon uptake and storage
heat uptake from the atmosphere
separatedFrom Labrador Basin NERFINISHED
separatedFromBy Greenland–Scotland Ridge NERFINISHED
studiedInField climate science
physical oceanography
tectonicSetting formed by seafloor spreading in the North Atlantic
waterMassTransformation subpolar mode water formation region

Referenced by (1)

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

Irminger Sea seaFloorFeature Irminger Basin