Alboran gyre

E143589

The Alboran gyre is a large, persistent rotating ocean current system in the western Mediterranean that strongly influences water circulation, mixing, and ecosystem dynamics in the Alboran Sea.

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All labels observed (2)

Label Occurrences
Alboran gyre canonical 1
Mediterranean circulation system 1

Statements (30)

Predicate Object
instanceOf ocean gyre
oceanographic feature
physical oceanographic phenomenon
affects biological productivity in the Alboran Sea
distribution of nutrients in the Alboran Sea
heat distribution in the western Mediterranean
plankton distribution in the Alboran Sea
drivenBy exchange between Atlantic Ocean and Mediterranean Sea
hasCharacteristic large
persistent
rotating current system
hasEffect formation of ocean fronts in the Alboran Sea
retention of water masses in the Alboran Sea
hasMedium seawater
hasProcess horizontal mixing
vertical mixing
hasRelevanceFor biogeochemical cycles in the Alboran Sea
fisheries in the Alboran Sea
regional climate of the western Mediterranean
hasTemporalStability quasi-permanent
influences ecosystem dynamics in the Alboran Sea
water circulation in the Alboran Sea
water mixing in the Alboran Sea
locatedIn Alboran Sea
Western Mediterranean
surface form: western Mediterranean Sea
occursIn surface ocean layer
partOf Alboran gyre self-linksurface differs
surface form: Mediterranean circulation system
relatedTo Strait of Gibraltar inflow
studiedInField marine ecology
physical oceanography

Referenced by (2)

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

Alboran Sea oceanographicFeature Alboran gyre
Alboran gyre partOf Alboran gyre self-linksurface differs
this entity surface form: Mediterranean circulation system