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The existence small-scale inhomogeneities in cumulus clouds leads to a reinterpretation of the experimental data on total water mixing ratio Q and wet equivalent potential temperature θq. This reinterpretation indicates that the height of the level of entrained air may be sometimes overestimated.
The existence small-scale inhomogeneities in cumulus clouds leads to a reinterpretation of the experimental data on total water mixing ratio Q and wet equivalent potential temperature θq. This reinterpretation indicates that the height of the level of entrained air may be sometimes overestimated.
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