Water and ammonia abundances in S140 with the Odin satellite

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Table B.3:

H₂O Gaussian fits^a. $T_{\rm b}$ (PDR) uses a source size of 120 $^{\prime \prime }$ $\rightarrow \eta _{\rm bf}$ = 2, while $T_{\rm b}$ (outflow) uses a source size of 85 $^{\prime \prime }$ $\rightarrow \eta _{\rm bf}$ = 3.
Pos.	$\upsilon_{{\rm LSR}}$	err	$T^{~*}_{{\rm A}}$	$T_{\rm b}$	err	$\Delta \upsilon$	err
	[km s^-1]	[km s^-1]	[mK]	[mK]	[mK]	[km s^-1]	[km s^-1]
1	-7.5	0.10	180	400	12	3.1	0.2
2	-6.9	0.08	340	756	28	3.5	0.3
	-5.4	0.39	171	570	27	8.8	0.7
3	-7.1	0.06	416	924	30	3.1	0.20
	-6.1	0.24	213	710	31	8.8	0.60
4	-7.1	0.08	316	702	44	3.5	0.4
	-6.6	0.8	78	260	45	10.0	4.1

^a Notation as in Table B.2.

Source LaTeX | All tables | In the text

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