Equation of state for solar near-surface convection

Numerical 3-D radiative hydrodynamical simulations are the main tool for the analysis of the interface between the solar convection zone and the photosphere. The equation of state is one of the necessary ingredients of these simulations. We compare two equations of state that are commonly used, o...

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Main Authors: N. Vitas, E. Khomenko
Format: Article
Language:English
Published: Copernicus Publications 2015-06-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/33/703/2015/angeo-33-703-2015.pdf
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spelling doaj-75305d6fe034411cb3271c6d71867aaa2020-11-24T23:16:15ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762015-06-013370370910.5194/angeo-33-703-2015Equation of state for solar near-surface convectionN. Vitas0N. Vitas1E. Khomenko2E. Khomenko3E. Khomenko4Universidad de La Laguna, Dpto. Astrofísica, 38206 La Laguna, Tenerife, SpainInstituto de Astrofísica de Canarias, C/ Via Lactea S/N, 38200 La Laguna, Tenerife, SpainMain Astronomical Observatory, Academy of Sciences Ukraine, Golosiiv, Kiev 22, 252650, UkraineUniversidad de La Laguna, Dpto. Astrofísica, 38206 La Laguna, Tenerife, SpainInstituto de Astrofísica de Canarias, C/ Via Lactea S/N, 38200 La Laguna, Tenerife, SpainNumerical 3-D radiative hydrodynamical simulations are the main tool for the analysis of the interface between the solar convection zone and the photosphere. The equation of state is one of the necessary ingredients of these simulations. We compare two equations of state that are commonly used, one ideal and one nonideal, and quantify their differences. Using a numerical code we explore how these differences propagate with time in a 2-D convection simulation. We show that the runs with different equations of state (EOSs) and everything else identical relax to statistically steady states in which the mean temperature (in the range of the continuum optical depths typical for the solar photosphere) differs by less than 0.2%. For most applications this difference may be considered insignificant.https://www.ann-geophys.net/33/703/2015/angeo-33-703-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. Vitas
N. Vitas
E. Khomenko
E. Khomenko
E. Khomenko
spellingShingle N. Vitas
N. Vitas
E. Khomenko
E. Khomenko
E. Khomenko
Equation of state for solar near-surface convection
Annales Geophysicae
author_facet N. Vitas
N. Vitas
E. Khomenko
E. Khomenko
E. Khomenko
author_sort N. Vitas
title Equation of state for solar near-surface convection
title_short Equation of state for solar near-surface convection
title_full Equation of state for solar near-surface convection
title_fullStr Equation of state for solar near-surface convection
title_full_unstemmed Equation of state for solar near-surface convection
title_sort equation of state for solar near-surface convection
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2015-06-01
description Numerical 3-D radiative hydrodynamical simulations are the main tool for the analysis of the interface between the solar convection zone and the photosphere. The equation of state is one of the necessary ingredients of these simulations. We compare two equations of state that are commonly used, one ideal and one nonideal, and quantify their differences. Using a numerical code we explore how these differences propagate with time in a 2-D convection simulation. We show that the runs with different equations of state (EOSs) and everything else identical relax to statistically steady states in which the mean temperature (in the range of the continuum optical depths typical for the solar photosphere) differs by less than 0.2%. For most applications this difference may be considered insignificant.
url https://www.ann-geophys.net/33/703/2015/angeo-33-703-2015.pdf
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