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The courses of the warm Agulhas current (red) along the east coast of South Africa, and the cold Benguela current (blue) along the west coast, originating in the Indian Ocean and Atlantic Ocean respectively. Note that the Benguela current does not originate from Antarctic waters in the South Atlantic Ocean, but from upwelling of water from the cold depths of the Atlantic Ocean against the west coast of the continent. The two currents do not "meet" anywhere along the south coast of Africa.
The courses of the warm Agulhas current (red) along the east coast of South Africa, and the cold Benguela current (blue) along the west coast, origina
The red areas show major upwelling areas. The Benguela Current is on the southwest coast of Africa.
The red areas show major upwelling areas. The Benguela Current is on the southwest coast of Africa.
Unusually strong winds from the east push warm (red) surface water towards Africa, allowing cold (blue) water to upwell along the Sumatran coast
Unusually strong winds from the east push warm (red) surface water towards Africa, allowing cold (blue) water to upwell along the Sumatran coast
During an El Niño, wind indirectly drives warm water to the South American coast, reducing the effects of cold upwelling.
During an El Niño, wind indirectly drives warm water to the South American coast, reducing the effects of cold upwelling.
Aerial view of Slapton Sands and northern part of Ley geograph.org.uk 1434412
Aerial view of Slapton Sands and northern part of Ley geograph.org.uk 1434412
Maldivesfish 2
Maldivesfish 2