The shape-velocity alignment of satellites forged by tidal locking and dynamical friction
Hao Yang, Wenting Wang, Ting S. Li, Sergey E. Koposov, Jiaxin Han, Feihong He, Zhaozhou Li, Zhongxu Zhai, Binbin Gao, Carles G. Palau, Zhenlin Tan
TL;DR
This study uses the high-resolution TNG50 simulation to quantify two intrinsic alignment signals for satellites and subhalos: radial alignment of their major axes with galactocentric directions and orbital alignment with their velocity vectors. It finds strong radial alignment, especially for subhalos, largely insensitive to host halo mass, and a weaker but significant orbital alignment that varies with orbital phase and halo mass due to dynamical friction and tidal stripping. The authors show that observed MW-like alignment signals in projection can largely arise from the coplanarity of major axes with orbital planes, amplified for highly elliptical systems. Together, the results link tidal torque, orbit decay, and tidal streams to orientation statistics, with implications for interpreting weak-lensing systematics and halo assembly histories.
Abstract
Utilizing the TNG50 simulation, we study two types of alignments for satellites/subhalos: 1) the alignment of their major axes with the galactocentric radial directions (radial alignment), and 2) with the motion directions (orbital alignment). We find that radial alignment is substantially stronger than orbital alignment, with both signals being consistently stronger for subhalos than for satellites. Interestingly, inward- and outward-moving satellites/subhalos show contrasting orbital alignment behaviors, which can be understood in terms of their radial alignment, orbit decay due to dynamical friction and the effect of tidal stripping. The orbital alignment is stronger in more massive halos. In the end, we explore the orbital alignment measured by a mock observer, and find that the alignment reported by Pace et al. (2022) for MW satellites is due to projection effects, as the major axes of satellites lie within their orbital planes, approximately coplanar with the observer.
