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Table 2:

WD atmosphere model plus MEKAL fits to V598 Pup spectra at three epochs.
Satellite Day since No. of counts Atmos. kT Atmos. fluxa MEKAL kT MEKAL kT MEKAL fluxa C-stat/d.o.f.
  Optical peak in spectrum (eV) (erg cm-2 s-1) (eV) (eV) (erg cm-2 s-1)  
XMM 147 MOS1: 653 35 $\pm$ 1b (8.1 $\pm$ 0.3) $\times$ 10-12 $\rm 187^{+14}_{-12}$ $\rm 788^{+92}_{-86}$ (3.0 $\pm$ 0.4) $\times$ 10-13 383/342
    MOS2: 641            
    pn: 3458            
Swift 172 117 $\rm 63^{+5}_{-4}$ $\rm 8.9^{+3.2}_{-2.2}$ $\times$ 10-13 $\rm 636^{+218}_{-335}$ - $\rm 1.7^{+0.7}_{-0.5}$ $\times$ 10-13 76/56
Swift 247 88 $\rm 68^{+>18}_{-5}$ $\rm 2.0^{+0.7}_{-0.5}$ $\times$ 10-13 $\rm 608^{+153}_{-144}$ - $\rm 8.3^{+2.6}_{-3.1}$ $\times$ 10-14 39/54

The day since peak corresponds to the mid-time of the spectrum. The absorbing column was fixed at 4.8 $\times$ 1020 cm-2 (Read et al. 2008). The XMM-Newton EPIC MOS1, MOS2 and pn spectra were fitted simultaneously, with a free constant of normalisation between them: with the pn constant fixed to unity, MOS 1 and MOS 2 have constants of 0.91 $\pm$ 0.08 and 0.96 $\pm$ 0.08 respectively. The temperature of the WD atmosphere component for the day 247 observation is constrained by the upper limit allowed by the model.
a Unabsorbed, over 0.3-10 keV.
b A systematic error of up to 25% may be required in addition; see text for details.

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