Liman Current

E12641

Liman Current is a cold ocean current flowing southwestward along the northwestern coast of the Sea of Japan, influencing the region’s climate and marine conditions.


Statements (36)
Predicate Object
instanceOf cold current
ocean current
affects marine ecosystems in the northwestern Sea of Japan
sea ice distribution in the northwestern Sea of Japan
sea surface temperature in the northwestern Sea of Japan
associatedWith enhanced biological productivity
high nutrient levels
borderedBy Russian Far East coast
contrastsWith Tsushima Current
contributesTo cooling of coastal air temperatures along the Russian coast of the Sea of Japan
formation of cold water masses in the northwestern Sea of Japan
drivenBy density gradients in the Sea of Japan
regional wind patterns over the Sea of Japan
flowDirection southwestward
flowsAlong northwestern coast of the Sea of Japan
flowsNear Primorsky Krai coast
Tatar Strait region
hasNameOrigin named after Liman Bay region of the Russian Far East
hasSeasonalVariation stronger in winter
weaker in summer
hasTemperatureCharacteristic cold
hasWaterMassProperty low surface temperature relative to surrounding waters
relatively low salinity compared to adjacent warm currents
influences distribution of fish stocks in the northwestern Sea of Japan
distribution of plankton in the northwestern Sea of Japan
fog formation along the Russian coast of the Sea of Japan
local fisheries in the northwestern Sea of Japan
marine conditions of the northwestern Sea of Japan
regional climate of the northwestern Sea of Japan
vertical mixing in the northwestern Sea of Japan
interactsWith Tsushima Current
locatedIn Northwest Pacific Ocean
Sea of Japan
partOf circulation system of the Sea of Japan
studiedInDiscipline marine climatology
physical oceanography

Referenced by (1)
Subject (surface form when different) Predicate
Sea of Japan
hasCurrent

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