The equations of motion for moist atmospheric air
Anastassia M. Makarieva, Victor G. Gorshkov, Andrei V. Nefiodov,, Douglas Sheil, Antonio D. Nobre, Peter Bunyard, Paulo Nobre, Bai-Lian Li

TL;DR
This paper clarifies the equations of motion for moist atmospheric air, resolving a controversy over the 'reactive motion' term by distinguishing assumptions for condensation and evaporation, and providing a revised equation.
Contribution
It offers a new, generally applicable equation for moist air motion, clarifying the role of phase transitions and correcting misconceptions about reactive motion.
Findings
Reactive motion does not occur during condensation.
The 'reactive motion' term applies only to evaporation, not condensation.
A revised equation for moist air motion is proposed.
Abstract
How phase transitions affect the motion of moist atmospheric air remains controversial. In the early 2000s two distinct differential equations of motion were proposed. Besides their contrasting formulations for the acceleration of condensate, the equations differ concerning the presence/absence of a term equal to the rate of phase transitions multiplied by the difference in velocity between condensate and air. This term was interpreted in the literature as the "reactive motion" associated with condensation. The reasoning behind this "reactive motion" was that when water vapor condenses and droplets begin to fall the remaining gas must move upwards to conserve momentum. Here we show that the two contrasting formulations imply distinct assumptions about how gaseous air and condensate particles interact. We show that these assumptions cannot be simultaneously applicable to condensation and…
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