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.

All labels observed (1)

Label Occurrences
Irminger Basin canonical 1

How this entity was disambiguated

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 ⓘ
Reykjanes Ridge ⓘ
southeast Greenland continental margin ⓘ
circulationInfluencedBy East Greenland Current ⓘ
Irminger Current ⓘ
circulationType cyclonic subpolar gyre circulation ⓘ
connectedTo Iceland Basin ⓘ
Labrador Sea ⓘ
countryExclusiveEconomicZones Greenland ⓘ
Iceland ⓘ
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 ⓘ
Irminger Sea Intermediate Water ⓘ
Labrador Sea Water ⓘ
importantFor deep water formation in the North Atlantic ⓘ
ventilation of the subpolar gyre ⓘ
isPartOf Greenland–Iceland–Norwegian Seas–North Atlantic system ⓘ
linked to: Nordic Seas
locatedIn North Atlantic Ocean ⓘ
linked to: North Atlantic
locatedSoutheastOf Greenland ⓘ
locatedUnder Irminger Sea ⓘ
locatedWestOf Iceland ⓘ
maximumDepth approximately 3000–3500 m ⓘ
namedAfter Carl Ludvig Christian Irminger ⓘ
near Denmark Strait ⓘ
oceanRegion Labrador–Irminger Seas region ⓘ
linked to: Labrador Sea
partOf Atlantic Meridional Overturning Circulation ⓘ
North Atlantic subpolar gyre ⓘ
subpolar North Atlantic ⓘ
roleInClimate carbon uptake and storage ⓘ
heat uptake from the atmosphere ⓘ
separatedFrom Labrador Basin ⓘ
separatedFromBy Greenland–Scotland Ridge ⓘ
studiedInField climate science ⓘ
physical oceanography ⓘ
tectonicSetting formed by seafloor spreading in the North Atlantic ⓘ
waterMassTransformation subpolar mode water formation region ⓘ

How these facts were elicited

Referenced by (1)

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

Irminger Sea → seaFloorFeature → Irminger Basin ⓘ