Mann Eddy: Difference between revisions
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{{short description|A persistent clockwise circulation in the middle of the North Atlantic ocean}} |
{{short description|A persistent clockwise circulation in the middle of the North Atlantic ocean}} |
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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.<ref>{{cite web |url=http://www.agu.org/cgi-bin/SFgate/SFgate?language=English&verbose=0&listenv=table&application=fm10&convert=&converthl=&refinequery=&formintern=&formextern=&transquery=bingham&_lines=&multiple=0&descriptor=%2fdata%2fepubs%2fwais%2findexes%2ffm10%2ffm10%7c761%7c2560%7cUsing%20GOCE%20to%20estimate%20the%20mean%20North%20Atlantic%20circulation%20%28%3Ci%3EInvited%3C%2fi%3E%29%7cHTML%7clocalhost:0%7c%2fdata%2fepubs%2fwais%2findexes%2ffm10%2ffm10%7c21927386%2021929946%20%2fdata2%2fepubs%2fwais%2fdata%2ffm10%2ffm10.txt |title=Using GOCE to estimate the mean North Atlantic circulation (Invited) |author=Bingham, R J|year=2010 |work=Abstract presented at 2010 Fall Meeting, AGU, San Francisco, Calif., 13-17 Dec. |publisher=American Geophysical Union |accessdate=2010-12-22|display-authors=etal}} |
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." |
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<ref>{{cite web |url=http://www.agu.org/cgi-bin/SFgate/SFgate?language=English&verbose=0&listenv=table&application=fm10&convert=&converthl=&refinequery=&formintern=&formextern=&transquery=bingham&_lines=&multiple=0&descriptor=%2fdata%2fepubs%2fwais%2findexes%2ffm10%2ffm10%7c761%7c2560%7cUsing%20GOCE%20to%20estimate%20the%20mean%20North%20Atlantic%20circulation%20%28%3Ci%3EInvited%3C%2fi%3E%29%7cHTML%7clocalhost:0%7c%2fdata%2fepubs%2fwais%2findexes%2ffm10%2ffm10%7c21927386%2021929946%20%2fdata2%2fepubs%2fwais%2fdata%2ffm10%2ffm10.txt |title=Using GOCE to estimate the mean North Atlantic circulation (Invited) |author=Bingham, R J|year=2010 |work=Abstract presented at 2010 Fall Meeting, AGU, San Francisco, Calif., 13-17 Dec. |publisher=American Geophysical Union |accessdate=2010-12-22|display-authors=etal}} |
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<ref>{{cite web |url=https://www.bbc.co.uk/news/science-environment-11867162 |title=Goce gravity mission traces ocean circulation |author=Jonathan Amos, Science correspondent, BBC News |date= 21 Dec 2010 |work=BBC News website, Science & Environment |publisher=BBC News |accessdate=21 Dec 2010}}</ref> |
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== References == |
== References == |
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Revision as of 09:51, 14 September 2020
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)
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