Atlantic Meridional Overturning Circulation slowdown cooled the subtropical ocean.

Geophys Res Lett · 2013 · PMC4459181 · PMID 26074634

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a significant trendno p-value reported

Extending the reference period to the end of the MHT time series by definition results in no net change in OHC due to the integrated MHT divergence and atmospheric fluxes but forces a significant trend in OHC throughout the time series (section S2).

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