Radiation Hydrodynamics in Solar Flares

TL;DR

This paper models the complex interactions of energy transport, plasma heating, and shock formation during solar flares, providing insights into chromospheric evaporation and observable spectral signatures.

Contribution

It introduces a detailed radiation hydrodynamics model of solar flare phenomena, emphasizing chromospheric evaporation and shock dynamics, with testable observational predictions.

Findings

Downward moving chromospheric condensation decays after about one minute.

Supersonic downflows can generate radiating shocks that excite UV emission.

Predicted relationships between optical/UV spectra and shock dynamics.

Abstract

Solar flares are currently understood as the explosive release of energy stored in the form of stressed magnetic fields. In many cases, the released energy seems to take the form of large numbers of electrons accelerated to high energies or alternatively plasma heated to very high temperatures. The transport of this energy into the remaining portion of the atmosphere results in violent mass motion and strong emission across the electromagnetic spectrum. One important phenomenon observed during flares is the appearance in coronal magnetic loops of large amounts of upflowing, soft X-ray emitting plasma. It is believed that this is due to chromospheric evaporation, the process of heating cool chromospheric material beyond its ability to radiate. The pressure increase in the evaporated plasma leads to a number of interesting phenomena in the flare chromosphere. The sudden pressure increase initiates a downward moving "chromospheric condensation", an overdense region which gradually decelerates as it accretes material and propagates into the gravitationally stratified chromosphere. Solutions to an equation of motion for this condensation shows that its motion decays after about one minute of propagation into the chromosphere. When the front of this downflowing region is supersonic relative to the atmosphere ahead of it, a radiating shock will form. If the downflow is rapid enough, the shock strength should be sufficient to excite UV radiation normally associated with the transition region, and furthermore, the radiating shock will be brighter than the transition region. These results lead to a number of observationally testable relationships between the optical and ultraviolet spectra from the condensation and radiating shock.