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. 2021 Dec 15;7(51):eabi8230. doi: 10.1126/sciadv.abi8230

Fig. 2. Upstream and downstream path of the North Atlantic Current in the Arctic.

Fig. 2.

(A) Reconstructed August temperature in the Vøring Plateau (25), compared to AMV. (B) High-resolution IRD on the Eastern Fram Strait [core MSM5/5-712 (28)]. The IRD data were detrended to remove the neoglacial cooling trend. (C) C. neoteretis, a proxy for warm Atlantic waters in Western Fram Strait (core PS93/025) (29). (D) N. labradorica, a proxy for chilled Atlantic waters from core PS2641-4 (30) and IRD reported in Denmark Strait (32). The AMV is filtered by a 21-year Gaussian filter, and the gray-shaded area is the 95% confidence level of the reconstruction (23).