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Table 6:

The brightest lines predicted by models 1 and 6 (the model with the largest water abundance) compared with the upper limits derived by the ISO observations.)
    Model 1 Model 6 ISO  
Wavelength Transition Intensity Intensity Instrument Upper limit (3$\sigma$)
($\mu $m) $J_{K_- K_+} \rightarrow$ J'K'- K'+ (erg s-1 cm-2) (erg s-1 cm-2)   (erg s-1 cm-2)
ortho          
75.4957 8 $_{5 4} \rightarrow$ 84 5 2.6E-20 1.9E-19 LWS04 9.78e-12
108.073 2 $_{ 2 1} \rightarrow $ 11 0 1.3E-12 1.5E-12 LWS04 2.21e-12
179.527 2 $_{ 1 2} \rightarrow $ 10 1 1.2E-12 7.0E-12 LWS04 2.56e-11
113.538 4 $_{ 1 4} \rightarrow $ 30 3 8.3E-13 8.7E-13 LWS01 1.2e-11
para          
100.983 2 $_{ 2 0} \rightarrow $ 11 1 7.3E-13 9.1E-13 LWS01 8.37e-12
138.527 3 $_{ 1 3} \rightarrow $ 20 2 7.3E-13 7.3E-13 LWS01 4.14e-12
156.197 3 $_{2 2} \rightarrow$ 31 3 2.2E-13 3.4E-13 LWS01 1.60e-12


Source LaTeX | All tables | In the text

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