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Table B.2

Comparison of the methods and observation properties between this study and other outflow studies.

This study Bontemps et al. (1996) Sekimoto et al. (1997)

12CO line 3–2 2–1 2–1; 1–0
Sourcesa All EL 29, IRS 43, IRS 44, WL 6, WL 12 EL 29, IRS 44, WL 6
Beam size (″) 15 30(NRAO), 10(IRAM) 34
Map size (″×″) 120 × 120 60 × 60(NRAO), 25 × 25(IRAM) 68 × 68
Velocity res. (km s-1) 0.1 0.65(NRAO), 0.26(IRAM) 0.06; 0.05
σrms (K) 0.15 0.25(NRAO), 0.15(IRAM) 0.2; 0.15
Method νmax (M1) annulus (M6) νmax (M1)
νin off-source Tpeak/10 unknown
νout 1σ cut-off 1σ cut-off unknown
Opacity corr. none mean of CB92: 3.5 derived from 13CO: ~3.0(2–1)
Inclination corr. factors CB92 average i = 57.3: factor 2.9 factors CB92
Distance to Oph (pc) 120 160 160
Other Average off-source spectrum subtracted
before integration, integration
radius 45″(IRS 44), 15″(others)
Kamazaki et al. (2003) Bussmann et al. (2007) Nakamura et al. (2011)

12CO line 3–2 3–2 3–2
Sourcesa Elias 32/33 EL 29, LFAM 26 Elias 29, Elias 32/33b, LFAM 26
Beam size (″) 14 11 40
Map size (″×″) 120 × 240 (OphB2) 300 × 300 23′ × 23′
Velocity res. (km s-1) 0.33 0.4 0.4
σrms (K) 0.79 (OphB2) 0.4 0.28
Method ⟨ ν ⟩ (M3) νmax (M1) νmax (M1)
νin channel mapsc unknown channel maps
νout 3σ cut-off unknown 3σ cut-off
Opacity corr. 5.4d none none
Inclination corr. average i = 57.3: factor 2.9 none , i = 80 (El 29, LFAM 26), i = 57.3 (El 32)
Distance to Oph (pc) 160 120 125
Other

Notes.

(a)

Only the sources relevant for this study are listed in this table.

(b)

Elias 32 was adopted by Nakamura et al. (2011) as the driving source for this outflow, where Elias 33 was adopted in this study.

(c)

By determining integration limits using channel maps, the outflow emission is defined as the emission showing bipolar structure in a channel map. This is equivalent to the method used in this study, comparing off-source spectra with outflow spectra.

(d)

The factor 5.4 is based on the mean factor 3.5 as used in Bontemps et al. (1996), multiplied by 1.6 because the optical depth of the 3–2 transition is 1.6 times larger than the 2–1 transition of the latter (Kamazaki et al. 2003).

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