Dependence of on metallicity, intensity, and spatial scale in a self-regulated interstellar medium
arXiv:2201.03885 · doi:10.3847/1538-4357/ac65fd
Abstract
We study the CO(1-0)-to-H conversion factor () and the line ratio of CO(2-1)-to-CO(1-0) () across a wide range of metallicity () in high-resolution (~0.2 pc) hydrodynamical simulations of a self-regulated multiphase interstellar medium. We construct synthetic CO emission maps via radiative transfer and systematically vary the "observational" beam size to quantify the scale dependence. We find that the kpc-scale can be over-estimated at low if assuming steady-state chemistry or assuming that the star-forming gas is H-dominated. On parsec scales, varies by orders of magnitude from place to place, primarily driven by the transition from atomic carbon to CO. The pc-scale drops to the Milky Way value of once dust shielding becomes effective, independent of . The CO lines become increasingly optically thin at lower , leading to a higher . Most cloud area is filled by diffuse gas with high and low , while most CO emission originates from dense gas with low and high . Adopting a constant strongly over- (under-)estimates H in dense (diffuse) gas. The line intensity negatively (positively) correlates with () as it is a proxy of column density (volume density). On large scales, and are dictated by beam averaging, and they are naturally biased towards values in dense gas. Our predicted is a multivariate function of , line intensity, and beam size, which can be used to more accurately infer the H mass.
arXiv commentPublished in ApJ (typos in the abstract fixed). Code for interpolating Lagrangian (particle) data onto an adaptive mesh (and auxiliary scripts for RADMC-3D) available at https://github.com/huchiayu/ParticleGridMapper.jl
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