The XCO conversion factor from galactic multiphase ISM simulations

Abstract

CO(J=1-0) line emission is a widely used observational tracer of molecular gas, rendering essential the XCO factor, which is applied to convert CO luminosity to H2 mass. We use numerical simulations to study how XCO depends on numerical resolution, non-steady-state chemistry, physical environment, and observational beam size. Our study employs 3D magnetohydrodynamics (MHD) simulations of galactic disks with solar neighborhood conditions, where star formation and the three-phase interstellar medium (ISM) are self-consistently regulated by gravity and stellar feedback. Synthetic CO maps are obtained by post-processing the MHD simulations with chemistry and radiation transfer. We find that CO is only an approximate tracer of H2. On parsec scales, WCO is more fundamentally a measure of mass-weighted volume density, rather than H2 column density. Nevertheless, XCO =0.7-1.0×1020~cm-2K-1km-1s consistent with observations, insensitive to the evolutionary ISM state or radiation field strength if steady-state chemistry is assumed. Due to non-steady-state chemistry, younger molecular clouds have slightly lower XCO and flatter profiles of XCO versus extinction than older ones. The CO-dark H2 fraction is 26-79 %, anti-correlated with the average extinction. As the observational beam size increases from 1 pc to 100 pc, XCO increases by a factor of ~ 2. Under solar neighborhood conditions, XCO in molecular clouds is converged at a numerical resolution of 2 pc. However, the total CO abundance and luminosity are not converged even at the numerical resolution of 1 pc. Our simulations successfully reproduce the observed variations of XCO on parsec scales, as well as the dependence of XCO on extinction and the CO excitation temperature.

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