Mann Eddy

From Wikipedia, the free encyclopedia
Jump to: navigation, search

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.[1][2]


  1. ^ 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. 
  2. ^ Jonathan Amos, Science correspondent, BBC News (21 December 2010 Last updated at 00:10). "Goce gravity mission traces ocean circulation". BBC News website, Science & Environment. BBC News. Retrieved 21 Dec 2010.  Check date values in: |date= (help)