Atomic Carbon Is a Temperature Probe in Dark Clouds

Details Atomic Carbon Is a Temperature Probe in Dark Clouds Atomic Carbon Is a Temperature Probe in Dark Clouds

1999-06-17

arxiv.org/abs/astro-ph/9906284v1

Astronomy and Astrophysics

Astrophysics

2 pages, 16 PS figures, uses aaspp4.sty; Astrophys. J., in press

Scientific paper

10.1086/307991

We have mapped the C I 3P1-3P0 line at 492 GHzin three molecular clouds immersed in weak ultraviolet radiation fields, TMC-1, L134N, and IC 5146. In all three clouds, the CI peak TA* ~ 1 K, with very small dispersion. The spatial C I distribution is extended and rather smooth. The J = 2-1 transitions of CO isotopomers were observed at the same angular resolution as C I. The C I peak TA* is typically a third of the peak TA* of 13CO J = 2-1, and the C I emission is usually more extended than emission in 13CO or C18O J=2-1. The C I linewidth is close to the 13CO J = 2-1 linewidth, larger than the C18O J = 2-1 line width, and smaller than the 12CO J = 2-1 linewidth. The uniformity of the C I peak TA* is remarkable for a line in the Wien portion of the Planck function and indicates a very uniform excitation temperature. This uniformity is best explained if the line if opaque and thermalized. If so, the CI line probes kinetic temperature in clouds exposed to low ultraviolet fluxes. This conclusion has significant implications for the thermal balance in such clouds. At Av ~ 2, these clouds have a remarkably constant temperature from place to place and from cloud to cloud (7.9+/-0.8 K). Photodissociation region models of clouds immersed in the mean interstellar radiation field tend to predict stronger lines than we see, but this may be an artifact of assumptions about the temperature.

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