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. 2003 Dec 1;100(25):14655–14660. doi: 10.1073/pnas.2532677100

Fig. 2.

Fig. 2.

Ice concentrations nucleated by or within aerosol particles as a function of water vapor supersaturation (Upper) and ice supersaturation (Lower) for the project period. Data are color-coded to differentiate measurements in different temperature regimes. Increases in nucleated concentrations at near water saturation and at higher ice supersaturation conditions are indicative of homogeneous freezing at temperatures below –38°C.