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- Fig. 5: the total OHT through all Arctic straits increases in all experiments, again with a much more pronounced increase in the 2 wide domain experiments; the OHT increase in the Bering Strait experiment is stronger than in the northeastern Pacific experiment, in agreement with the sea-ice area/volume results;
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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 Fran 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. 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. 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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