Carbon monoxide in the solar atmosphere II. Radiative cooling by CO lines

TL;DR

This study investigates the cooling effect of carbon monoxide in the solar atmosphere's mid-photospheric to low-chromospheric layers, finding that CO cooling is too slow to significantly influence the dynamic thermal structure.

Contribution

It incorporates CO radiative cooling into a hydrodynamics code and assesses its impact on the solar atmosphere's thermal structure and dynamics.

Findings

CO cooling causes additional cooling at shock fronts.

Average temperature reduction is about 100 K due to CO cooling.

CO cooling is too slow to explain very cool regions in the solar atmosphere.

Abstract

The role of carbon monoxide as a cooling agent for the thermal structure of the mid-photospheric to low-chromospheric layers of the solar atmosphere in internetwork regions is investigated. The treatment of radiative cooling via spectral lines of carbon monoxide (CO) has been added to the radiation chemo-hydrodynamics code CO5BOLD. [...] The CO opacity indeed causes additional cooling at the fronts of propagating shock waves in the chromosphere. There, the time-dependent approach results in a higher CO number density compared to the equilibrium case and hence in a larger net radiative cooling rate. The average gas temperature stratification of the model atmosphere, however, is only reduced by roughly 100 K. Also the temperature fluctuations and the CO number density are only affected to small extent. A numerical experiment without dynamics shows that the CO cooling process works in principle and drives the atmosphere to a cool radiative equilibrium state. At chromospheric heights, the radiative relaxation of the atmosphere to a cool state takes several 1000 s. The CO cooling process thus would seem to be too slow compared to atmospheric dynamics to be responsible for the very cool temperature regions observed in the solar atmosphere. The hydrodynamical timescales in our solar atmosphere model are much too short to allow for the radiative relaxation to a cool state, thus suppressing the potential thermal instability due to carbon monoxide as a cooling agent. Apparently, the thermal structure and dynamics of the outer model atmosphere are instead determined primarily by shock waves.