Observed and simulated estimates of the meridional overturning circulation at 26.5 degrees N in the Atlantic
Daily timeseries of the meridional overturning circulation (MOC) estimated from the UK/US RAPID/MOCHA array at 26.5° [26.5 degrees] N in the Atlantic are used to evaluate the MOC as simulated in two global circulation models: (I) an 8-member ensemble of the coupled climate model ECHAM5/MPI-OM, and (...
Main Authors: | , , , , , |
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Other Authors: | |
Format: | Article |
Language: | en_US |
Published: |
European Geosciences Union / Copernicus
2011
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Online Access: | http://hdl.handle.net/1721.1/65382 https://orcid.org/0000-0003-3925-6161 |