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Table 3:

Properties of rotational water lines, and calculated line fluxes $F_L=\int (F_\nu-F_\nu^{\rm cont})~{\rm d}\nu$ for different line transfer methods.

Carrier
Transition $\lambda~[\mu$m] $A_{\rm ul}~[{\rm s}^{-1}]$ $E_u{\rm [K]}$ LTE ES MC |ES-MC|
o-H2O 110$~\to~$101 538.29 0.0035 61 0.702 0.531 0.538 2%
o-H2O 423$~\to~$312$^\star$ 180.49 0.0306 194 9.27 2.32 3.39 37%
o-H2O 212$~\to~$101$^\star$ 179.53 0.0559 114 11.9 7.69 8.59 11%
o-H2O 303$~\to~$212 174.63 0.0505 197 12.7 7.47 8.88 17%
o-H2O 212$~\to~$110 108.07 0.256 194 54.8 11.4 17.9 44%
o-H2O 423$~\to~$312$^\star$ 78.74 0.484 432 94.5 24.6 35.9 37%
p-H2O 202$~\to~$111 303.46 0.0058 101 1.27 1.48 1.40 5%
p-H2O 111$~\to~$000 269.27 0.0184 53 2.40 2.22 2.09 6%
p-H2O 413$~\to~$322$^\star$ 144.52 0.0332 397 5.53 4.57 4.15 9%
p-H2O 313$~\to~$202 138.53 0.125 204 14.3 7.76 8.71 12%
p-H2O 220$~\to~$111 100.98 0.260 196 32.5 8.66 10.9 23%
p-H2O 322$~\to~$211$^\star$ 89.99 0.352 297 48.0 10.2 14.0 31%
Listed line fluxes are in units 10-18 W/m2 for distance 140 pc and inclination $30^\circ $. $^\star$ Indicates that this line will be observed by the Herschel OT Key Programme GASPS. ES = escape probability, MC = Monte Carlo.

Source LaTeX | All tables | In the text

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