Dependence of regional ocean heat uptake on anthropogenic warming scenarios.

In the subpolar North Atlantic, the averaged OHU increases rapidly before 2050 (0.139 W m −2 year −1 , P < 0.01) and levels off or declines slightly after that, which corresponds to a positive trend of 0.045 W m −2 year −1 ( P < 0.01) during 2006–2100.

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Under the RCP2.6 scenario, OHU exhibits generally opposite trends between hemispheres: a significant positive trend in the subpolar North Atlantic but a negative trend in the Southern Ocean during 2006–2100 ( Fig. 1A ).

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