Examining the physical principles behind the motion of moist air: Which expressions are sound?
A. M. Makarieva, V. G. Gorshkov, A. V. Nefiodov, D. Sheil, A. D., Nobre, P. Bunyard, B.-L. Li

TL;DR
This paper critically examines two conflicting formulations of moist air motion equations, clarifies misconceptions about reactive motion, and emphasizes the importance of consistent momentum conservation in atmospheric modeling.
Contribution
It clarifies the physical principles behind moist air motion equations, refutes the reactive motion concept, and highlights the need for consistent momentum treatment in models.
Findings
Reactive motion concept is based on a misunderstanding of momentum conservation.
The mixed equation used in some models is physically inconsistent.
Total momentum consideration clarifies the correct formulation.
Abstract
The physical equations determining the motion of moist atmospheric air in the presence of condensation remain controversial. Two distinct formulations have been proposed, published and cited. The equation of Bannon [2002, J. Atmos. Sci. 59: 1967--1982] includes a term for a "reactive motion" that arises when water vapor condenses and droplets begin to fall; according to this term the remaining gas moves upwards so as to conserve momentum. In the equation of Ooyama[2001, J. Atmos. Sci. 58: 2073--2102] the reactive motion term is absent. Both equations contain a term for condensate loading, but in the formulation of Ooyama [2001] there are two additional terms. In some modern nonhydrostatic models of moist atmospheric circulation, however, formulations have been mixed. Here we examine the contrasting equations for the motion of moist air. We discuss inconsistencies in the application of…
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Taxonomy
TopicsMeteorological Phenomena and Simulations · Tropical and Extratropical Cyclones Research · Geophysics and Gravity Measurements
