CO and CS in the Magellanic Clouds: ax(2)-analysis of multitransitional data based on the MEP radiative transfer model

Abstract

Aims. Our goal is to determine the physical properties of molecular gas located in different environments of the SMC-from near the vicinity of hot HII regions to cold, quiescent clouds - via modelling and simulations, and compare with the properties of molecular gas found in similar environments in the LMC. Methods. We present observations of the (CO)-C-12(1-0), (2-1), (3-2), (CO)-C-13(1-0), (2-1), and CS (2-1), (3-2) line emission toward six molecular clouds in the SMC: N66, N88, Lirs 36, Lirs 49, Hodge 15, and SMC- B1# 1. These data, as well as published data on three clouds of the LMC: 30Dor- 10, N 159- W, and N159- S, are analysed to estimate gas kinetic temperatures, column densities, and surface filling factors using a Mean Escape Probability approximation of the radiative transfer equations. The solutions are restricted using the chi(2) approach. Results. Assuming that the [(CO)-C-12/(CO)-C-13] abundance ratio is similar in both galaxies, we find that the CO and CS column densities of SMC clouds are a magnitude smaller than those of LMC clouds, mirroring the metallicity differences. Our analysis suggests the existence of a lower limit for the (CO)-C-12/ (CO)-C-13 isotope ratio of 50 in both galaxies. The surface filling factors of the CO emission in the SMC clouds are a factor of a few smaller than in the LMC and seem to decrease with increasing UV radiation fields, i. e., more vigorous star formation activity. A simple model, which assumes a spherical cloud with uniform physical parameters immersed in the CMB radiation field, provides a reasonably good fit to the observed properties of the ( supposedly) quiescent clouds SMC- B1# 1 and N159- S. For all other clouds considered, this model gives large values of chi(2), strongly indicating the need for a more complex model. We present some results from 2- component modelling, e. g., for Lirs 36 a mixture of 20 K gas with high optical depth and a less dense gas with temperatures of 100 K reproduces well the main features of the CO data.