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Reversed flow of Atlantic deep water during the Last Glacial Maximum [1]

Additional image:: 

The meridional overturning circulation (MOC) of the Atlantic Ocean is considered to be one of the most important components of the climate system.

Publication Date: 
03/11/2010
Rainer Zahn [2], Csar Negre [3], Alexander L. Thomas & et al [4]
Nature [5]
468
7320
84
Tags:
North Atlantic Ocean [6], Climate Change [7], Climate Science [8], Oceans and Seas [9]

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Source URL: http://admin.indiaenvironmentportal.org.in/feature-article/reversed-flow-atlantic-deep-water-during-last-glacial-maximum

Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/reversed-flow-atlantic-deep-water-during-last-glacial-maximum
[2] http://admin.indiaenvironmentportal.org.in/category/author/rainer-zahn
[3] http://admin.indiaenvironmentportal.org.in/category/author/csar-negre
[4] http://admin.indiaenvironmentportal.org.in/category/author/alexander-l-thomas-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/journal/nature
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/north-atlantic-ocean
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/oceans-and-seas