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Statements

Subject Item
dbr:Agulhas_Leakage
rdfs:label
Agulhas Leakage
rdfs:comment
The Agulhas Leakage is an inflow of anomalously warm and saline water from the Indian Ocean into the South Atlantic due to the limited latitudinal extent of the African continent compared to the southern extension of the subtropical super gyre in the Indian Ocean. The process occurs during the retroflection of the Agulhas Current via shedding of anticyclonic Agulhas Rings, cyclonic eddies and direct inflow. The leakage contributes to the Atlantic Meridional Overturning Circulation (AMOC) by supplying its upper limb, which has direct .
foaf:depiction
n5:Agulhas_sea_surface_height.gif n5:Agulhas_surface_current_velocity.gif n5:Agulhas_surface_temperature.gif n5:Agulhas_pathway.png
dcterms:subject
dbc:Climate_of_Africa dbc:Currents_of_the_Indian_Ocean
dbo:wikiPageID
70333148
dbo:wikiPageRevisionID
1097267810
dbo:wikiPageWikiLink
dbr:Wind_stress dbr:Indian_Ocean dbr:Eddy_(fluid_dynamics) dbr:North_Brazil_Current dbr:Loop_Current dbr:Anthropogenic_climate_change dbr:Subtropical_front dbr:Benguela_Current dbr:Planetary_wave dbr:Inertia dbr:Paleoceanography dbr:Drake_Passage dbr:Westerlies dbr:Western_Boundary_Current dbc:Climate_of_Africa dbr:Atlantic_meridional_overturning_circulation dbr:Sverdrup dbr:South_Equatorial_Current dbr:Eddy_kinetic_energy dbr:Pleistocene dbr:Gulf_Stream dbr:Interglacial dbr:Subtropical_gyre dbr:Warm_core_ring n15:Agulhas_pathway.png dbr:Buoyancy dbr:North_Atlantic_Deep_Water n15:Agulhas_surface_current_velocity.gif dbr:Paleoclimatology dbr:Retroflect dbr:Cold_water_route dbr:Cape_Agulhas dbr:Agulhas_Current dbr:Instability dbr:Atlantic_Ocean dbr:Antarctic_Circumpolar_Current dbr:Isotopes_of_strontium dbr:Boundary_current dbr:Globorotalia_menardii dbr:Isotope_ratio dbr:Anticyclonic_rotation dbc:Currents_of_the_Indian_Ocean
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dbo:thumbnail
n5:Agulhas_pathway.png?width=300
dbo:abstract
The Agulhas Leakage is an inflow of anomalously warm and saline water from the Indian Ocean into the South Atlantic due to the limited latitudinal extent of the African continent compared to the southern extension of the subtropical super gyre in the Indian Ocean. The process occurs during the retroflection of the Agulhas Current via shedding of anticyclonic Agulhas Rings, cyclonic eddies and direct inflow. The leakage contributes to the Atlantic Meridional Overturning Circulation (AMOC) by supplying its upper limb, which has direct .
prov:wasDerivedFrom
wikipedia-en:Agulhas_Leakage?oldid=1097267810&ns=0
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16739
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wikipedia-en:Agulhas_Leakage