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Directory UMM :Data Elmu:jurnal:A:Atmospheric Research:Vol52.Issue1-2.Aug1999:

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Fig. 1. a Supersaturation change in continental cloud predicted by the present cloud model
Fig. 2. a Comparison of the maximum supersaturation in continental clouds predicted by the present cloudŽ .a function of updraft velocity.maximum supersaturation in maritime clouds predicted by the present model with Maxwellian and diffusion-kinetic drople
Fig. 3. Comparison of the maximum supersaturation in clouds for maritime CCN spectrum,.T Ns125Ž S-11r3.Supersaturation predicted by the present cloud model and Twomey’s and Fukuta–Xu’s analytical formulas aregiven, as a function of updraft velocity, all us
Fig. 4. Comparison of the maximum supersaturation in clouds for maritime spectrum, Ns160Ž S-1.1r4,predicted by the present cloud model and analytical formulas of Twomey and Fukuta–Xu with the Maxwelliandroplet growth theory
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