Figure 3
From: Ice nucleation active particles are efficiently removed by precipitating clouds
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).
