Extended Data Fig. 7: Reversal in summer \({{\boldsymbol{p}}}_{{{\bf{CO}}}_{{\bf{2}}}}^{{\prime} }\) is driven by a threefold increase in summer T′, while other changes are much smaller. | Nature

Extended Data Fig. 7: Reversal in summer \({{\boldsymbol{p}}}_{{{\bf{CO}}}_{{\bf{2}}}}^{{\prime} }\) is driven by a threefold increase in summer T′, while other changes are much smaller.

From: Arctic Ocean annual high in \({{\boldsymbol{p}}}_{{{\bf{CO}}}_{{\bf{2}}}}\) could shift from winter to summer

Extended Data Fig. 7

Arctic domain averages of monthly anomalies of the CMIP5 mean under RCP8.5 are shown for the modern (2006–2015, solid) and future (2091–2100, dashed) climatologies for the four driving variables: sAT′ (cyan), sCT′ (green), T′ (blue), and S′ (red). The shading indicates model spread (±1 s.d., n = 9), which for sAT′ and sCT′ is shown only for the future.

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