Mann Eddy
The Mann Eddy is a very small feature of ocean currents in the Atlantic. It is a persistent clockwise circulation in the middle of the North Atlantic ocean. The oceanographer Dr Rory Bingham from Newcastle University (UK) describes it as "a persistent pocket of water in the Atlantic that just goes around and around." [1] [2]
References
- ^ Bingham, R J; et al. (2010). "Using GOCE to estimate the mean North Atlantic circulation (Invited)". Abstract presented at 2010 Fall Meeting, AGU, San Francisco, Calif., 13-17 Dec. American Geophysical Union. Retrieved 2010-12-22.
- ^ Jonathan Amos, Science correspondent, BBC News (21 Dec 2010). "Goce gravity mission traces ocean circulation". BBC News website, Science & Environment. BBC News. Retrieved 21 Dec 2010.
{{cite web}}:|author=has generic name (help)CS1 maint: multiple names: authors list (link)
 | This article about a specific ocean current is a stub. You can help Wikipedia by expanding it. |