Antarctic Bottom Water circulation
GPTKB entity
Statements (23)
| Predicate | Object |
|---|---|
| gptkbp:instanceOf |
oceanographic phenomenon
|
| gptkbp:affects |
climate change
global ocean circulation melting Antarctic ice |
| gptkbp:characterizedBy |
cold temperatures
high salinity |
| gptkbp:contributedTo |
gptkb:thermohaline_circulation
|
| gptkbp:discoveredBy |
oceanographers in the 20th century
|
| gptkbp:form |
deepest water mass in the world ocean
|
| https://www.w3.org/2000/01/rdf-schema#label |
Antarctic Bottom Water circulation
|
| gptkbp:importantFor |
carbon sequestration
nutrient transport |
| gptkbp:influenced |
deep ocean currents
|
| gptkbp:monitors |
oceanographic research vessels
|
| gptkbp:movesToward |
northward from Antarctica
|
| gptkbp:notableDriver |
formation of dense water near Antarctica
|
| gptkbp:occurredIn |
gptkb:Southern_Ocean
|
| gptkbp:reach |
gptkb:Atlantic_Ocean
gptkb:Indian_Ocean gptkb:Pacific_Ocean |
| gptkbp:relatedTo |
gptkb:Antarctic_Bottom_Water
|
| gptkbp:bfsParent |
gptkb:Vema_Channel
|
| gptkbp:bfsLayer |
7
|