Seasonal variability of the Atlantic Meridional Overturning Circulation at 26.5 degrees N
The Atlantic meridional overturning circulation (AMOC) makes the strongest oceanic contribution to the meridional redistribution of heat. Here, an observation-based, 48-month-long time series of the vertical structure and strength of the AMOC at 26.5 degrees N is presented. From April 2004 to April...
Published in: | Journal of Climate |
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Main Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2010
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Subjects: | |
Online Access: | http://hdl.handle.net/11858/00-001M-0000-0011-F5A5-C http://hdl.handle.net/11858/00-001M-0000-0014-1A80-B |