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. 2016 Aug 15;113(35):9710–9715. doi: 10.1073/pnas.1524766113

Fig. S5.

Fig. S5.

Time series of the decomposition of the simulated local summer temperature anomaly at GISP2 (solid black line) into the contributions from local elevation change corrected by a lapse rate of 6.5 °C/km (gray line) and the regional summer temperature anomaly forcing (dashed line).