Propagating intensity disturbances in polar corona as seen from AIA/SDO

TL;DR

This study uses high-resolution AIA/SDO data to analyze quasi-periodic intensity disturbances in the polar corona, suggesting they are likely magneto-acoustic waves contributing to solar wind acceleration.

Contribution

It provides detailed observations of propagating disturbances in polar corona across multiple passbands, supporting their wave nature and multi-thermal characteristics.

Findings

Disturbances have periodicities of 10-30 min.

Propagation speeds range from 100-170 km/s.

Speeds vary between passbands and regions, indicating magneto-acoustic waves.

Abstract

Polar corona is often explored to find the energy source for the acceleration of the fast solar wind. Earlier observations show omni-presence of quasi-periodic disturbances, travelling outward, which is believed to be caused by the ubiquitous presence of outward propagating waves. These waves, mostly of compressional type, might provide the additional momentum and heat required for the fast solar wind acceleration. It has been conjectured that these disturbances are not due to waves but high speed plasma outflows, which are difficult to distinguish using the current available techniques. With the unprecedented high spatial and temporal resolution of AIA, we search for these quasi-periodic disturbances in both plume and interplume regions of the polar corona. We investigate their nature of propagation and search for a plausible interpretation. We also aim to study their multi-thermal nature by using three different coronal passbands of AIA. In almost all the locations chosen, in both plume and interplume regions we find the presence of propagating quasi-periodic disturbances, of periodicities ranging from 10-30 min. These are clearly seen in two channels and in a few cases out to very large distances (~250 arcsec) off-limb, almost to the edge of the AIA field of view. The propagation speeds are in the range of 100-170 km/s. The average speeds are different for different passbands and higher in interplume regions. Observed disturbances are insensitive to changes in slit width. This indicates that a coherent mechanism is involved. In addition, the observed propagation speed varies between the different passpands, implying that these quasi-periodic intensity disturbances are possibly due to magneto-acoustic waves. The propagation speeds in interplume region are higher than in the plume region.