1999
DOI: 10.1029/1998jc900099
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Indian‐Atlantic interocean exchange: Dynamics, estimation and impact

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Cited by 331 publications
(301 citation statements)
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“…We explored the possibility that recent dispersal by currents between the Atlantic and Indo-Paci® c could explain our ® ndings. Although this tropical species is highly unlikely to be able to disperse around Cape Horn (South America) due to the cold waters of the circum-Antarctic current, dispersal around the Cape of Good Hope (South Africa) may be more probable, as warm waters of the Agulhas current travelling south along the eastern side of South Africa are able tō ow into the southeastern Atlantic (Briggs 1974;Gordon 1985;de Ruijter et al 1999). However, the Benguela cold current, and upwelling off southwestern Africa, present a major barrier to the dispersal of even highly vagile tropical Indian Ocean taxa into the Atlantic (Bowen et al 2001).…”
Section: Discussionmentioning
confidence: 99%
“…We explored the possibility that recent dispersal by currents between the Atlantic and Indo-Paci® c could explain our ® ndings. Although this tropical species is highly unlikely to be able to disperse around Cape Horn (South America) due to the cold waters of the circum-Antarctic current, dispersal around the Cape of Good Hope (South Africa) may be more probable, as warm waters of the Agulhas current travelling south along the eastern side of South Africa are able tō ow into the southeastern Atlantic (Briggs 1974;Gordon 1985;de Ruijter et al 1999). However, the Benguela cold current, and upwelling off southwestern Africa, present a major barrier to the dispersal of even highly vagile tropical Indian Ocean taxa into the Atlantic (Bowen et al 2001).…”
Section: Discussionmentioning
confidence: 99%
“…The upper limb of the Atlantic MOC originates in the southeastern Atlantic where South Atlantic Current (SAC) water merges with Indian Ocean leakage in the Benguela Current (Reid, 1989;Peterson and Stramma, 1991;Stramma and England, 1999;de Ruijter et al, 1999) Accurate knowledge of the circulation patterns in the southeastern Atlantic and of the amounts of water from different sources in the Benguela Current has remained lacking because of the complexities of the ocean circulation and the sparse amount of suitable direct measurements.…”
Section: Scientific Backgroundmentioning
confidence: 99%
“…Estimates of Agulhas leakage using geostrophic sections range from around 3-15 Sv (1 Sv = 10 6 m 3 /s), and estimates of leakage due to Agulhas rings range from around 3-9 Sv based on the formation of 6 rings per year each with a transport of 0.5 to 1.5 Sv (de Ruijter et al, 1999;Gordon, 2001). Estimates of the amount of intermediate water entering the Benguela Current from the Agulhas range from near zero (Rintoul, 1991) to around 50% (Gordon et al, 1992).…”
Section: Scientific Backgroundmentioning
confidence: 99%
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