Fig. 3 | Nature Communications

Fig. 3

From: Seasonal energy exchange in sea ice retreat regions contributes to differences in projected Arctic warming

Fig. 3

Seasonality of partial temperature contributions. Seasonal cycles of (a) surface albedo feedback, (b) cloud radiative effect, (c) ocean heat storage, and (d) surface turbulent flux partial temperature contributions averaged over the Arctic domain (60°–90° N). The gray shaded region denotes the ensemble mean (solid black line) +/− one standard deviation

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