Comments on "MSE minus CAPE is the True Conserved Variable for an Adiabatically Lifted Parcel"
Pascal Marquet

TL;DR
This paper critiques Romps (2015) by clarifying assumptions, correcting the interpretation of CAPE, and proposing more accurate thermodynamic formulations for moist air using the third law.
Contribution
It clarifies the hypotheses in Romps (2015), corrects the interpretation of CAPE, and introduces improved thermodynamic formulas based on the third law of thermodynamics.
Findings
CAPE in R15 is opposite of the actual convective available energy.
Vertical adiabatic ascent in R15 is unrealistic due to water condensation.
More precise moist-air thermodynamic functions can be derived using the third law.
Abstract
In a recent paper, Romps (JAS, vol.72, p.3639-3646, 2015, hereafter R15) argues that the moist-air static energy (MSE) is only approximately conserved for an adiabatically lifted parcel, and that the quantity "MSE - CAPE" could be used as a true conserved variable, where CAPE is the convective available energy. It is shown in this comment that the quantity denoted by CAPE in R15 is the opposite of the convective available energy. It is explained that the vertical adiabatic ascent considered in R15 is not realistic, since it generates condensed water of the order of 10 to 20 g/kg at height above 6 km. Moreover, the thermodynamic equations are written in R15 by making several assumptions, not all of which are explicitly mentioned. This comment aims to clarify the hypotheses made in R15. It will show that these assumptions call into question the validity of the moist-air internal…
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