Shear-gravity transition determines the steep velocity dispersion-size relation in molecular clouds: confronting analytical formula with observations
Yi-Heng Xie, Guang-Xing Li

TL;DR
This paper introduces a two-component model combining gravity and shear to explain the steep velocity dispersion-size relation observed in molecular clouds, highlighting a transition at around 100 parsecs.
Contribution
The study presents a novel two-component model that accounts for both gravity and shear effects, explaining the observed steep velocity dispersion-size relation in molecular clouds.
Findings
Small clouds' velocity dispersion is dominated by self-gravity.
Large clouds' velocity dispersion is primarily influenced by shear.
A transition scale of about 100 pc links the two regimes.
Abstract
The velocity dispersion-size relation () is a crucial indicator of the dynamic properties of interstellar gas, where the slope is considered as . Recent observations reveal a steep velocity dispersion-size relation with the slope , which cannot be explained by a single mechanism with only gravity () or shear (). We present a two-component model to explain the steep velocity dispersion-size relation for clouds larger than several parsecs in observations from e.g. Miville-Desch\^{e}nes et al. (2017), Zhou et al. (2022) and Sun et al. (2024). We find that, above several parsecs, the velocity dispersion of small clouds is mainly caused by self-gravity, while large clouds…
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Taxonomy
TopicsAstrophysics and Star Formation Studies · Cold Atom Physics and Bose-Einstein Condensates · Astro and Planetary Science
