Table A.1:

Summary of o-H218O 110 - 101 model results.

Envelope abundance
$T_{\rm MB}^{\rm peak}$ $\int T_{\rm MB}~{\rm d}\varv$
Inner Outer (K) (K km s-1)

$1\times 10^{-5}$
$3 \times 10^{-10}$ 0.017 0.071
$3 \times 10^{-6}$ $3 \times 10^{-10}$ 0.018 0.075
$1 \times 10^{-6}$ $3 \times 10^{-10}$ 0.017 0.069
$3\times 10^{-7}$ $3 \times 10^{-10}$ 0.016 0.065
$1\times 10^{-7}$ $3 \times 10^{-10}$ 0.015 0.060
$3 \times 10^{-8}$ $3 \times 10^{-10}$ 0.014 0.054
$1 \times 10^{-8}$ $3 \times 10^{-10}$ 0.014 0.050

$1\times 10^{-5}$
$2 \times 10^{-10}$ 0.015 0.063
$3 \times 10^{-6}$ $2 \times 10^{-10}$ 0.014 0.060
$1 \times 10^{-6}$ $2 \times 10^{-10}$ 0.014 0.060
$3\times 10^{-7}$ $2 \times 10^{-10}$ 0.013 0.052

$1\times 10^{-5}$
$1 \times 10^{-10}$ 0.010 0.043
$1 \times 10^{-6}$ $1 \times 10^{-10}$ 0.009 0.038
$3\times 10^{-7}$ $1 \times 10^{-10}$ 0.009 0.036
$1\times 10^{-7}$ $1 \times 10^{-10}$ 0.008 0.032
$3 \times 10^{-8}$ $1 \times 10^{-10}$ 0.007 0.027

Notes. The observed line has a $T_{\rm MB}^{\rm peak} = 0.015$ K and an $\int T_{\rm MB}~{\rm d}\varv = 0.071$ K km-1, the best fitting model is selected by comparison with the latter.


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