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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 33, issue 6
Ann. Geophys., 33, 703–709, 2015
https://doi.org/10.5194/angeo-33-703-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Observation, analysis and modelling of solar and heliospheric...

Ann. Geophys., 33, 703–709, 2015
https://doi.org/10.5194/angeo-33-703-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Regular paper 09 Jun 2015

Regular paper | 09 Jun 2015

Equation of state for solar near-surface convection

N. Vitas2,1 and E. Khomenko3,2,1 N. Vitas and E. Khomenko
  • 1Instituto de Astrofísica de Canarias, C/ Via Lactea S/N, 38200 La Laguna, Tenerife, Spain
  • 2Universidad de La Laguna, Dpto. Astrofísica, 38206 La Laguna, Tenerife, Spain
  • 3Main Astronomical Observatory, Academy of Sciences Ukraine, Golosiiv, Kiev 22, 252650, Ukraine

Abstract. 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.

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