Molecular and Atomic Gas in the Large Magellanic Cloud - I. Conditions for CO Detection
T. Wong (1, 2), A. Hughes (3, 2), Y. Fukui (4), A. Kawamura (4),, N. Mizuno (4, 5), J. Ott (6, 7), E. Muller (4, 2), J. L. Pineda (9),, D. E. Welty (1), S. Kim (9), Y. Mizuno (4), M. Murai (4), T. Onishi (4) ((1), U. of Illinois, (2) CSIRO ATNF, (3) Swinburne, (4) Nagoya U.

TL;DR
This study investigates the conditions under which CO emission is detectable in the Large Magellanic Cloud, revealing that high HI density and temperature are necessary but not sufficient, and exploring factors influencing molecular cloud formation.
Contribution
It provides new insights into the variability of CO detection conditions and examines the roles of HI properties and environmental factors in molecular cloud formation in the LMC.
Findings
High HI column density and brightness are necessary for CO detection.
Significant scatter in CO intensity persists even at large spatial scales.
Large HI linewidths may suppress CO emission, indicating warm HI's role.
Abstract
We analyze the conditions for detection of CO(1-0) emission in the Large Magellanic Cloud (LMC), using the recently completed second NANTEN CO survey. In particular, we investigate correlations between CO integrated intensity and HI integrated intensity, peak brightness temperature, and line width at a resolution of 2.6' (~40 pc). We find that significant HI column density and peak brightness temperature are necessary but not sufficient conditions for CO detection, with many regions of strong HI emission not associated with molecular clouds. The large scatter in CO intensities for a given HI intensity persists even when averaging on scales of >200 pc, indicating that the scatter is not solely due to local conversion of HI into H_2 near GMCs. We focus on two possibilities to account for this scatter: either there exist spatial variations in the I(CO) to N(H_2) conversion factor, or a…
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