Calculations of the ascent of a saturate
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B. J. Mason; R. Emig
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Article
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1961
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John Wiley and Sons
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English
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## Abstract Numerical computations are made to show how the vertical velocity, temperature, humidityβmixing ratio and liquidβwater content of a cloudy parcel will vary with height and time as it ascends from the condensation level, rises through, and mixes with, the surrounding environment whose te