Articles | Volume 24, issue 2
https://doi.org/10.5194/hess-24-967-2020
https://doi.org/10.5194/hess-24-967-2020
Research article
 | 
28 Feb 2020
Research article |  | 28 Feb 2020

Impacts of non-ideality and the thermodynamic pressure work term pΔv on the surface energy balance

William J. Massman

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (07 Oct 2019) by Stan Schymanski
AR by William J Massman on behalf of the Authors (24 Oct 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (09 Nov 2019) by Stan Schymanski
RR by Grant Petty (15 Nov 2019)
RR by Anonymous Referee #1 (27 Nov 2019)
RR by Andrew Kowalski (13 Dec 2019)
ED: Publish subject to minor revisions (review by editor) (10 Jan 2020) by Stan Schymanski
AR by William J Massman on behalf of the Authors (16 Jan 2020)  Author's response   Manuscript 
ED: Publish as is (23 Jan 2020) by Stan Schymanski
AR by William J Massman on behalf of the Authors (29 Jan 2020)
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Short summary
Studies of the surface energy balance of the earth (SEB) often show that measured incoming energy exceeds the sum of measured outgoing energy terms. The present study models two contributions to the outgoing terms of the SEB: (a) water vapor and dry air as non-ideal gases and (b) the contribution of evaporation to the convective heat. As anticipated, the results are insufficient to resolve the closure mystery, but they should provide insights into atmospheric thermodynamics and the SEB.