Fig. 2: Impact of high water vapor supersaturation on aerosol activation. | npj Climate and Atmospheric Science

Fig. 2: Impact of high water vapor supersaturation on aerosol activation.

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

Fig. 2: Impact of high water vapor supersaturation on aerosol activation.

a Relationship between supersaturation (SS), aerosol hygroscopicity (κ), and the critical dry diameter for activation (Ddc). The dashed box highlights the high-probability density function (PDF) region of observed κ and SS, corresponding to the distribution range of Ddc. b PDF of Ddc and its occurrence probability across different size ranges.

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