Propagating waves along spicules

TL;DR

This study analyzes the properties of Alfvénic waves along solar spicules in a polar coronal hole, revealing complex wave behaviors including upward, downward, and standing waves, with implications for solar atmospheric seismology.

Contribution

Developed an automated detection technique for spicules and waves, providing detailed statistical analysis of wave propagation modes and their variation with height.

Findings

Detected 89 spicules with mixed wave modes

Phase speed increases with height

Upward waves dominate at lower altitudes

Abstract

Alfv\'enic waves are thought to play an important role in coronal heating and acceleration of solar wind. Here we investigated the statistical properties of Alfv\'enic waves along spicules (jets that protrude into the corona) in a polar coronal hole using high cadence observations of the Solar Optical Telescope (SOT) onboard \emph{Hinode}. We developed a technique for the automated detection of spicules and high-frequency waves. We detected 89 spicules, and found: (1) a mix of upward propagating, downward propagating, as well as standing waves (occurrence rates of 59%, 21%, and 20%, respectively). (2) The phase speed gradually increases with height. (3) Upward waves dominant at lower altitudes, standing waves at higher altitudes. (4) Standing waves dominant in the early and late phases of each spicule, while upward waves were dominant in the middle phase. (5) In some spicules, we find waves propagating upward (from the bottom) and downward (from the top) to form a standing wave in the middle of the spicule. (6) The medians of the amplitude, period, and velocity amplitude were 55 km, 45 s, and 7.4 km s$^{-1}$, respectively. We speculate that upward propagating waves are produced near the solar surface (below the spicule) and downward propagating waves are caused by reflection of (initially) upward propagating waves off the transition region at the spicule top. The mix of upward and downward propagating waves implies that exploiting these waves to perform seismology of the spicular environment requires careful analysis and may be problematic.