A self-consistent 3D MHD model producing a solar blowout jet
Yajie Chen, Hardi Peter, Damien Przybylski, Lakshmi Pradeep Chitta, Sudip Mandal
TL;DR
The paper addresses how solar blowout jets can form through self-consistent magneto-convective dynamics rather than prescribed surface drivers. It uses a 3D radiation MHD model with the MURaM code to let a twisted flux tube emerge through the photosphere and reconnect with open field, transferring twist via interchange reconnection. The simulation reproduces a standard jet that transitions into a blowout jet with a fast heating front traveling at the local Alfvén speed and a slower mass upflow, matching observed speeds and timing; synthetic emissions in EUV and X-ray channels concur with observations. The results provide a physically grounded mechanism for blowout jets and reveal how near-surface convection-generated magnetic structures can drive energy release and twist transfer to the solar wind base.
Abstract
Context. Solar blowout jets are a distinct subclass of ubiquitous extreme-ultraviolet (EUV) and X-ray coronal jets. Aims. Most existing models of blowout jets prescribe an initial magnetic field configurations and apply ad-hoc changes in the photosphere to trigger the jets. In contrast, we aim for a self-consistent magneto-convective description of the jet initiation. Methods. We employ a 3D radiation magnetohydrodynamic (MHD) model of a solar coronal hole region using the MURaM code. The computational domain extends from the upper convection zone to the lower corona. We synthesize the emission in the extreme UV and X-rays for a direct comparison to observations and examine the evolution of the magnetic field structure of the event. Results. In the simulation a twisted flux tube forms self-consistently, emerges through the surface and interacts with the pre-existing open field. Initially the resulting jet is of the standard type with a narrow spire. The release of the twist into the open field causes a broadening of the jet spire turning the jet into a blowout type. At the same time this creates a fast heating front propagating at the local Alfvén speed. The properties of the modeled jet closely match observations of blowout jets: a slow (180 km/s) mass upflow and a fast (500 km/s) propagating front form, the latter being a signature of the heating front. Also the timing of the jet with respect to the flux emergence and subsequent cancellation matches observations. Conclusions. The near-surface magneto-convection self-consistently generates a twisted flux tube that emerges through the photosphere. The tube then interacts with the pre-existing magnetic field by means of interchange reconnection. This transfers the twist to the open field region and produces a blowout jet that matches the main characteristics of this type of jet found in observations.
