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. 2015 Nov 10;5:16433. doi: 10.1038/srep16433

Figure 3. Ratio of INPs−10 to the total number of particles >0.5 μm (N>0.5, on log scale) as a function of the fraction of water vapour lost from the air mass prior to arrival at the observatory (n = 71, Spearman’s r = −0.42, p < 0.001).

Figure 3