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 (...
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European Geosciences Union / Copernicus,
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