Iceland–Scotland Overflow Water

E728851

Iceland–Scotland Overflow Water is a cold, dense deep-water mass that flows southward from the Nordic Seas across the Iceland–Scotland Ridge, contributing to the formation of North Atlantic Deep Water and the global thermohaline circulation.

Jump to: Surface forms Statements Referenced by

Observed surface forms (2)

Statements (40)

Predicate Object
instanceOf deep water mass
overflow water
water mass
contributesTo North Atlantic Deep Water NERFINISHED
global thermohaline circulation
crosses Iceland–Scotland Ridge NERFINISHED
flowsAlong deep western boundary current system of the North Atlantic
flowsDirection southward
formsBy brine rejection during sea-ice formation
cooling of Nordic Seas surface waters
increased density due to heat loss
hasDensity high
hasDepthRange deep ocean depths below the Iceland–Scotland Ridge sill
hasFormationRegion Greenland–Scotland Ridge region NERFINISHED
hasProperty higher temperature than Denmark Strait Overflow Water on average
less dense than Denmark Strait Overflow Water on average
hasRole feeds lower limb of Atlantic overturning circulation
hasSalinity relatively high
hasTemperature cold
hasTransportAcross Iceland–Scotland Ridge NERFINISHED
influences deep stratification of the North Atlantic
storage of carbon in the deep ocean
storage of heat in the North Atlantic
ventilation of the deep North Atlantic
isAffectedBy atmospheric forcing over the Nordic Seas
changes in sea-ice cover in the Nordic Seas
variability in the North Atlantic Oscillation
isComponentOf Nordic Seas overflows NERFINISHED
isDistinctFrom Denmark Strait Overflow Water NERFINISHED
isKeyFor climate variability in the North Atlantic region
long-term deep-ocean ventilation timescales
isMonitoredBy current meters
hydrographic sections
oceanographic moorings
locatedIn North Atlantic Ocean NERFINISHED
mixesWith Denmark Strait Overflow Water downstream
ambient North Atlantic intermediate waters
originatesIn Nordic Seas NERFINISHED
partOf Atlantic Meridional Overturning Circulation NERFINISHED
sinksTo deep ocean layers

Referenced by (4)

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

Denmark Strait overflow pathway associatedWith Iceland–Scotland Overflow Water
this entity surface form: Greenland-Scotland Ridge overflow system
Labrador Sea Water mixesWith Iceland–Scotland Overflow Water
Labrador Sea Water mixesWith Iceland–Scotland Overflow Water
this entity surface form: Denmark Strait Overflow Water
Denmark Strait overflow pathway waterMassType Iceland–Scotland Overflow Water
this entity surface form: Denmark Strait Overflow Water