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- Fig. 6: the OHT at the BSO increases in all experiments, but much more clearly in the North Atlantic experiment;
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- Fig. 7: the OHT at the Bering Strait increases in all experiments, but more markedly in the North Pacific and Bering Strait experiments;
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- Fig. 8: the OHT at the Fram Strait generally increases in the wide and middle domain experiments, but with much lower amplitude compared to the increased OHT at the BSO and Bering Strait.
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- Fig. 9: the AMOC index at 26.5N decreases in the wide and middle domain experiments, which partly explains the decreased OHT south of 60N;
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- Fig. 9: the annual mean AMOC index at 26.5N decreases in the wide and middle domain experiments, which partly explains the decreased OHT south of 60N;
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- Fig. 10: the Atlantic meridional stream function (AMSF) strongly decreases in the 2 wide domain experiments (left column), decreases in the 2 middle domain experiments (middle column), doesn't change much in the BSO experiment (top right panel) and increases in the Bering Strait experiment (bottom right panel); interestingly, in the wide domain experiments (left column), the AMSF increases in the upper layers north of 60N, which is in agreement with the increased OHT north of 60N (Fig. 1); the overall AMSF decrease in the first 2 columns is in agreement with the reduced convection already identified in the mixed layer depth in Fig. 8 of the Atlantic [SST restoring experiments](SST restoring experiments).
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**Fig. 1: Latitudinal transect of mean Atlantic OHT averaged over 50 years for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom) experiments; the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**
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**Fig. 8: Time series of ocean heat transport (OHT) at the Fram Strait for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom panel) experiments; the number in brackets is the difference in mean OHT between the experiment and the control (CTRL)**
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**Fig. 9: Time series of Atlantic Meridional Overturning Circulation (AMOC) index at 26.5N (maximum Atlantic meridional stream function between 900 and 1200m) for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom panel) experiments**
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**Fig. 9: Time series of annual mean Atlantic Meridional Overturning Circulation (AMOC) index at 26.5N (maximum Atlantic meridional stream function between 900 and 1200m) for the control run and the 3 Atlantic (top panel) and 3 Pacific (bottom panel) experiments**
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**Fig. 10: Vertical profiles of the difference in Atlantic meridional stream function (AMSF) between the Atlantic (top panel) / Pacific (bottom panel) experiments and the control run, averaged over 50 years** |
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**Fig. 10: Vertical profiles of the difference in the mean Atlantic meridional stream function (AMSF) between the Atlantic (top panel) / Pacific (bottom panel) experiments and the control run, averaged over 50 years** |
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