MOW

E733844

MOW is a dense, salty water mass originating from the Mediterranean Sea that flows into the Atlantic Ocean and significantly influences its thermohaline circulation.

All labels observed (1)

Label Occurrences
MOW canonical 1

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf Mediterranean water mass ⓘ
water mass ⓘ
affects density structure of the North Atlantic ⓘ
overturning circulation in the Atlantic ⓘ
contributesTo salinity maximum at intermediate depths in the North Atlantic ⓘ
exitsThrough Strait of Gibraltar ⓘ
flowsInto Atlantic Ocean ⓘ
formedBy evaporation in the Mediterranean Sea ⓘ
mixing of Mediterranean waters with Atlantic waters in the Strait of Gibraltar ⓘ
fullName Mediterranean Overflow Water ⓘ
hasAbbreviation MOW ⓘ
hasProperty high density ⓘ
high salinity ⓘ
relatively high temperature compared to surrounding deep waters ⓘ
influences thermohaline circulation of the Atlantic Ocean ⓘ
isAlsoCalled Mediterranean Outflow Water ⓘ
isDetectedBy salinity anomalies ⓘ
temperature anomalies ⓘ
tracer distributions ⓘ
isImportantFor climate system through its impact on Atlantic circulation ⓘ
isStudiedIn climate science ⓘ
physical oceanography ⓘ
mixesWith North Atlantic Central Water ⓘ
North Atlantic Deep Water ⓘ
originatesFrom Mediterranean Sea ⓘ
playsRoleIn redistribution of salt in the Atlantic Ocean ⓘ
ventilation of intermediate waters in the North Atlantic ⓘ
sinksTo intermediate depths in the Atlantic Ocean ⓘ
spreadsAlong eastern North Atlantic basin ⓘ
typicalDepthRange approximately 800–1500 meters ⓘ

How these facts were elicited

Referenced by (1)

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