Jump to content

Guinea Current

From Wikipedia, the free encyclopedia
The South Atlantic Gyre.

The Guinea Current is a slow warm water current that flows to the east along the Guinea coast of West Africa. It has some similarity to the Equatorial Counter Current in the Indian and Pacific Oceans.[1]

See also

[edit]

References

[edit]
  1. ^ Bakun, Andrew (January 1978). "Guinea Current upwelling". Nature. 271 (5641): 147–150. Bibcode:1978Natur.271..147B. doi:10.1038/271147a0. ISSN 1476-4687.