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The theory of the growth (or evaporation) of a stationary drop has been cast into a form which reveals explicitly the role of both condensation and thermal accommodation coefficients. The equations for growth are integrated under constant ambient conditions. An application to cloud physics is discussed.
The theory of the growth (or evaporation) of a stationary drop has been cast into a form which reveals explicitly the role of both condensation and thermal accommodation coefficients. The equations for growth are integrated under constant ambient conditions. An application to cloud physics is discussed.
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| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 272 | 61 | 29 |
| PDF Downloads | 26 | 13 | 0 |
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