Ratio of H2 0-0S(3) / 0-0S(1) Intensity Ratio (Z = 3) line intensities emitted from the surface of a PDR as a function of the cloud density n, and the FUV flux incident on the cloud G0 .     Models of Kaufman et al. 2006 are used.

Ratio of H<sub>2</sub> 0-0S(3) / 0-0S(1) Intensity Ratio (Z = 3) line intensities
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WITS PDRT DIRT UMD IRSA

Please direct comments, criticisms, corrections and contributions to Marc Pound.
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