Table 3
Observed and predicted water line fluxes for an OPR H2O = 3.
| LVG predictions | ||||||||
|
|
||||||||
| Line | Freq. | λ | Eu/kB | Flux[12.7′′]a | Comp. 1-warmb | Comp. 2-hotc | Total | |
| (GHz) | (μm) | (K) | (K kms-1) | (K kms-1) | (K kms-1) | (K kms-1) | ||
|
|
||||||||
| o-H 2 O | ||||||||
|
|
||||||||
| 110 − 101 | 556.936 | 538.66 | 26.7 | 35.0(13.0)d | 39.0 | 8.3 | 47.3 | |
| 312 − 303 | 1097.365 | 273.38 | 215.1 | 6.0(2.0) | 0.3 | 1.0 | 1.3 | |
| 312 − 221 | 1153.127 | 260.17 | 215.1 | 1.9(0.9) | 0.05 | 1.4 | 1.5 | |
| 321 − 312 | 1162.912 | 257.98 | 271.0 | 0.8(0.4) | 0.02 | 0.9 | 0.9 | |
| 221 − 212 | 1661.008 | 180.49 | 159.8 | 3.0(1.0) | 0.2 | 1.6 | 1.8 | |
| 212 − 101 | 1669.905 | 179.52 | 80.1 | 14.0(4.0) | 9.2 | 2.7 | 11.9 | |
| 303 − 212 | 1716.770 | 174.62 | 162.5 | 6.0(2.0) | 1.0 | 3.4 | 4.4 | |
| 414 − 303 | 2640.474 | 113.54 | 289.3 | 0.6(0.3) | 0.06 | 0.4 | 0.5 | |
| 212 − 110 | 2773.977 | 108.10 | 159.9 | 0.6(0.2) | 0.4 | 0.6 | 1.0 | |
|
|
||||||||
| p-H 2 O | ||||||||
|
|
||||||||
| 211 − 202 | 752.033 | 398.92 | 136.9 | 11.4(3.3) | 1.3 | 6.2 | 7.5 | |
| 202 − 111 | 987.927 | 303.67 | 100.8 | 19.0(6.0) | 2.9 | 8.4 | 11.3 | |
| 111 − 000 | 1113.343 | 269.47 | 53.4 | 21.0(6.0) | 12.8 | 6.3 | 19.1 | |
| 313 − 202 | 2164.132 | 138.54 | 207.7 | 1.1(0.3) | 0.1 | 1.0 | 1.1 | |
Notes. Uncertainties are indicated in parentheses.
LVG predicted fluxes for the best-fit model of the warm component (Tkin = 250 K, n(H2) = 106 cm-3, N(o-H2O) = 2 × 1014 cm-2, N(p-H2O) = 7.0 × 1013 cm-2, and a source size of 10′′) and using an OPR H2 of 0.5 (see Sects. 4.2.1. and 4.2.2).
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