Fig. 7: The effect of weak hygroscopicity on aerosol activation and indirect effects. | npj Climate and Atmospheric Science

Fig. 7: The effect of weak hygroscopicity on aerosol activation and indirect effects.

From: In-situ observations reveal weak hygroscopicity in the Southern Tibetan Plateau: implications for aerosol activation and indirect effects

Fig. 7

a Measured and predicted CCN number concentration (NCCN) at different supersaturation (SS) conditions; b Relative deviation between predicted and measured NCCN; c Relative deviation to cloud optical thickness (τ); d Relative deviation to the threshold function of the cloud‐to‐rain transition (Tauto).

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