Vertical structure and kinematics of the LMC disc from SDSS/Gaia

TL;DR

This study combines SDSS-IV/V and Gaia data to analyze the vertical structure and kinematics of the LMC disc, revealing it is warped and not a flat, equilibrium plane, with variations in inclination and orientation.

Contribution

It introduces a new method for constructing a continuous 3D model of the LMC disc and provides detailed insights into its warped, non-equilibrium structure using combined datasets.

Findings

LMC disc is warped and tilted, not flat.

Inner and outer disc regions have different inclinations.

The central bar is tilted relative to the outer disc.

Abstract

[Abbreviated] Context: Studies of the LMC's internal kinematics have provided a detailed view of its structure, largely by the exquisite proper motion data supplied by Gaia. However, LoS velocities are only available for a small subset of Gaia data, limiting studies of the kinematics perpendicular to the LMC disc plane. Aims: We synergise new SDSS-IV/V LoS velocity measurements with Gaia data, increasing the 5D phase-space sample by almost a factor of three. We interpret and model the vertical structure and kinematics of the LMC disc. Methods: Split our sample into different stellar types. Then examine maps of vertical velocity moments perpendicular to the LMC disc. We interpret our results within three possible scenarios: 1) time-variability in the orientation of the disc symmetry axis; 2) use of an incorrect LMC disc plane orientation; or 3) the presence of warps or twists in the LMC disc. We also present a new method to construct a continuous 3D representation of the disc from spatially-resolved measurements of its viewing angles. Results: Using young stellar populations, we identify a region in the LMC arm with highly negative v_z'; this overlaps spatially with the supershell LMC 4. Our results indicate that: 1) the LMC viewing angles may vary with time, but this cannot explain most of the structure in v_z' maps; 2) when re-deriving the LMC disc plane by minimising the RMS vertical velocity v_z' across the disc, the inclination and line-of-nodes position angle are i ~ 24 degr and \Omega ~ 327 degr, respectively; 3) we obtain different inclinations for the inner and outer disc regions, and a quadrupolar variation with azimuth in outer the disc. We provide 3D models of the LMC disc shape. Conclusions: The combination of SDSS-IV/V and Gaia data reveal that the LMC disc is not a flat plane in equilibrium, but that the central bar region is tilted relative to a warped outer disc.