An improved approximation for the moist-air entropy potential temperature $\theta_s$
Atmospheric and Oceanic Physics
2015-03-10 v1 Fluid Dynamics
Geophysics
Abstract
The moist-air entropy is defined in Marquet (QJRMS 2011, arXiv:1401.1097) by in terms of two constant values (, ) and a potential entropy temperature denoted by . It is shown in Marquet (2011) that a quantity denoted by plays the role of a leading order approximation of . The aim of this note is to demonstrate in a more rigorous way that is indeed the leading order approximation of , and to derive a second order approximation which may be used in computations of values, gradients or turbulent fluxes of moist-air entropy. Some impacts of this second order approximation are described in this brief version of a note to be submitted to the QJRMS.
Cite
@article{arxiv.1503.02287,
title = {An improved approximation for the moist-air entropy potential temperature $\theta_s$},
author = {Pascal Marquet},
journal= {arXiv preprint arXiv:1503.02287},
year = {2015}
}
Comments
2 pages, 3 figures, submitted for a WGNE "Blue Book" publication