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Table 2:

Overview of the emission of the SQ postshock gas, from observations and model predictionsa. The models are the same as those used in Fig. 5.
          F LUX OF S PECTRAL F EATURES (10-18 W m-2)
  Mass Flow $P/k_{\rm B}$ $V_{\rm s}$b Cooling Timec O I [$63~\mu$m] $\rm H_2$ rot.d $\rm H_2$ 1-0 S(1) O I 6300 Åe $\rm H_{\alpha}$e
  [$M_{\odot}$ yr-1] [K cm-3] [km s-1] [yr]
Observations           $55 \pm 3$   3.6 5.3
Isobaric Cooling 100 (WIM, H$_\alpha$)f $2 \times 10^5$   $1.2 \times 10^4$ 3.9 1.4 0.05 0.5 5.3
640 (WNM, O I)g $2 \times 10^5$   $1.5 \times 10^5$ 25.8 9.1 0.3 3.6 
Shock Models $5.7 \times 10^3$ $4.5 \times 10^7$ 5 $1.8 \times 10^4$ 13 27 0.3 10-5  
270 $5.6 \times 10^8$ 20 $3.7 \times 10^3$ 0.04 25 0.01 $5 \times 10^{-3}$ 
a All line fluxes are scaled to the aperture ${\cal A} = 11.3$ $\times $ 4.7 arcsec2. For isobaric cooling calculations, the pressure is set to the SQ postshock gas value. For MHD shock models, both contributions of the 2 shock velocities to the emission are indicated, as well as the pressure for the warm $\rm H_2$ phase in the shock.
b MHD Shock velocity.
c Cooling time computed down to 50 K.
d Sum of the $\rm H_2$ S(0) to S(5) rotational lines (from Appleton et al. 2006).
e From optical observations by Xu et al. (2003).
f Mass flow derived from H$~ \alpha$ observations, ignoring ionization. It represents the isobaric cooling of the recombining H II gas.
g Cooling mass flow derived from O I observations and model calculations at the ambient SQ pressure. This mass flow does not depend much on the pressure since the critical density of the O I line is high (2 $\times $ 106 cm-3).

Source LaTeX | All tables | In the text

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