Eurasian Arctic deep-water system
E539538
The Eurasian Arctic deep-water system is a major oceanographic region of the Arctic Ocean characterized by interconnected deep basins and water masses that influence global thermohaline circulation and climate.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Eurasian Arctic deep-water system canonical | 1 |
Statements (48)
| Predicate | Object |
|---|---|
| instanceOf |
deep-water system
ⓘ
marine environment ⓘ oceanographic region ⓘ |
| affectedBy |
changes in Atlantic inflow
ⓘ
climate change ⓘ sea-ice decline ⓘ |
| characterizedBy |
cold deep waters
ⓘ
distinct water masses ⓘ high stratification ⓘ interconnected deep basins ⓘ strong halocline ⓘ |
| connectedTo |
Barents Sea opening
NERFINISHED
ⓘ
Fram Strait NERFINISHED ⓘ Greenland Sea deep waters ⓘ |
| exportsWaterTo |
Greenland Sea
NERFINISHED
ⓘ
North Atlantic NERFINISHED ⓘ |
| hasComponent |
Amundsen Basin
NERFINISHED
ⓘ
Fram Strait deep passage NERFINISHED ⓘ Gakkel Ridge flanks ⓘ Nansen Basin NERFINISHED ⓘ |
| hasProcess |
deep-water formation modification
ⓘ
mixing across the Arctic halocline ⓘ ventilation of deep basins ⓘ |
| hasProperty |
high salinity in deep layers
ⓘ
long residence times of deep waters ⓘ low temperature ⓘ |
| hasRole |
buffering heat and salt in the Arctic Ocean
ⓘ
linking Arctic and North Atlantic deep waters ⓘ |
| hasWaterMass |
Arctic Intermediate Water
NERFINISHED
ⓘ
Atlantic Water layer ⓘ Eurasian Basin Bottom Water NERFINISHED ⓘ Eurasian Basin Deep Water NERFINISHED ⓘ |
| influences |
Arctic climate
ⓘ
Northern Hemisphere climate ⓘ global thermohaline circulation ⓘ |
| locatedIn |
Arctic Ocean
ⓘ
Eurasian Basin NERFINISHED ⓘ |
| partOf |
Arctic deep-water circulation
ⓘ
global ocean circulation ⓘ |
| receivesWaterFrom |
Atlantic Water inflow
ⓘ
Barents Sea branch of Atlantic inflow ⓘ Fram Strait branch of Atlantic inflow NERFINISHED ⓘ Nordic Seas NERFINISHED ⓘ |
| relevantFor |
carbon cycle in the Arctic Ocean
ⓘ
heat transport to the Arctic ⓘ sea-ice dynamics ⓘ |
| studiedIn |
climate science
ⓘ
physical oceanography ⓘ |
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.