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. 2015 Nov 19;5:16820. doi: 10.1038/srep16820

Figure 5. Linear correlation of the snow end date De anomalies with the TOA (a) SW flux, (b) LW flux and (c) Net flux over the NH snow covered landmass from 2001 to 2013.

Figure 5

SW, LW and Net flux were derived from CERES observations. Linear correlations in (a–c) are significant at the 95% CL.