Some further results on convective currents
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An earlier theory of steady state, saturated convective currents is modified to include the drag of the condensed liquid water on the rising air. The system of equations is numerically integrated for several cases in which the entrainment is allowed to assume negative values. Results appear to indicate improvement over the earlier model.
The article of record as published may be found at http://dx.doi.org/10.3402/tellusa.v12i4.9417