Observations of a pulse driven cool polar jet by SDO/AIA

TL;DR

This study combines observations and numerical simulations to demonstrate that a single velocity pulse triggered by low-atmospheric reconnection can produce a polar jet with observed properties in the solar atmosphere.

Contribution

It provides the first strong evidence linking a single velocity pulse to the formation of a polar jet, modeled using realistic solar temperature conditions.

Findings

Numerical simulations match observed jet velocities, height, and lifetime.

A single velocity pulse can generate the observed jet features.

Reconnection in the lower atmosphere likely triggers the velocity pulse.

Abstract

Context. We observe a solar jet at north polar coronal hole (NPCH) using SDO AIA 304 {\deg}A image data on 3 August 2010. The jet rises obliquely above the solar limb and then retraces its propagation path to fall back. Aims. We numerically model this observed solar jet by implementing a realistic (VAL-C) model of solar temperature. Methods. We solve two-dimensional ideal magnetohydrodynamic equations numerically to simulate the observed solar jet. We consider a localized velocity pulse that is essentially parallel to the background magnetic field lines and initially launched at the top of the solar photosphere. The pulse steepens into a shock at higher altitudes, which triggers plasma perturbations that exhibit the observed features of the jet. The typical direction of the pulse also clearly exhibits the leading front of the moving jet. Results. Our numerical simulations reveal that a large amplitude initial velocity pulse launched at the top of the solar photosphere produces in general the observed properties of the jet, e.g., upward and backward average velocities, height, width, life-time, and ballistic nature. Conclusions. The close matching between the jet observations and numerical simulations provides first strong evidence for the formation of this jet by a single velocity pulse. The strong velocity pulse is most likely generated by the low- atmospheric reconnection in the polar region which results in triggering of the jet. The downflowing material of the jet most likely vanishes in the next upcoming velocity pulses from lower solar atmosphere, and therefore distinctly launched a single jet upward in the solar atmosphere is observed.