Fig. 1: Statistical characterization of water vapor supersaturation in STP orographic clouds. | npj Climate and Atmospheric Science

Fig. 1: Statistical characterization of water vapor supersaturation in STP orographic clouds.

From: High effective supersaturation offsets low aerosol hygroscopicity to promote orographic cloud formation over the southern Tibetan Plateau

Fig. 1

a Mean effective supersaturation (SSeff) and supersaturation calculated from the CCN spectrum (SSCCN) for each cloud case. b Mean and standard deviation of SSeff and SSCCN, along with the probability density functions (PDFs). c Correlation between case-averaged SSeff and SSCCN, with the black line representing the linear fit.

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