Arctic Ocean Amplification in a warming climate in CMIP6 models.

Sci Adv · 2022 · PMC9328679 · PMID 35895818

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a positive trendno p-value reported

Subsequently, the sea surface heat flux averaged over the Arctic Ocean will present a positive trend (less heat loss; Fig. 3 ), primarily because of the notable positive trends during 2071–2100 in the Barents Sea, Kara Sea, Chukchi Sea, and Baffin Bay (fig.

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