An azimuthally resolved study of sloshing cold fronts in three nearby galaxy clusters
I-Hsuan Li, Shutaro Ueda, I-Non Chiu, Keiichi Umetsu
TL;DR
This study performs an azimuthally resolved X-ray analysis of sloshing cold fronts in three nearby clusters (A496, A2029, A1644) using Chandra residual maps to map edges along the sloshing spiral. By fitting a three-component density model to sector-based surface brightness profiles and combining with deprojected spectroscopy, it derives azimuthal profiles of density, temperature, pressure, and entropy contrasts across the fronts, denoted $j_n$, $j_T$, $j_p$, and $j_K$. The authors find that, in general, $j_p$ is below unity, indicating non-thermal pressure support beyond bulk flows; the azimuthal velocity gradients inferred from $j_p$ vary by cluster and do not align with a universal bulk-motion–driven mechanism. They conclude that magnetic fields, viscosity, or turbulence likely contribute to the front sharpness, and advocate for future XRISM measurements to directly probe ICM motions and test these non-thermal processes.
Abstract
We present a detailed analysis of sloshing cold fronts in a sample of three nearby galaxy clusters (Abell 496, Abell 2029, and Abell 1644) observed with the Chandra X-ray Observatory. Cold fronts manifest as sharp edges in the X-ray surface brightness of the intracluster medium (ICM) in galaxy clusters. In the residual X-ray surface brightness maps, where the global ICM distribution has been subtracted, cold fronts generated by gas sloshing are observed at the boundaries of the spiral excesses. We perform a systematic and comprehensive study of the surface brightness edges along the spiral excesses. We find the deficit of the thermal pressure radially inward of the brightness edges, in contrast to stripping cold fronts that typically exhibit higher thermal pressure in brightness edges. Assuming that the sharp edges in the X-ray surface brightness distributions are sustained entirely by the gas bulk motions, we estimate the velocity gradients across the edges that are required to compensate for the deficit of the thermal pressure. We do not find statistically significant velocity gradients along the azimuthal direction. Our results suggest that alternative mechanisms such as magnetic fields and viscosity are necessary to maintain the sharpness of sloshing cold fronts.
