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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 ![]() |
(8.1 ![]() ![]() |
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(3.0 ![]() ![]() |
383/342 |
MOS2: 641 | ||||||||
pn: 3458 | ||||||||
Swift | 172 | 117 |
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- |
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76/56 |
Swift | 247 | 88 |
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- |
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39/54 |
The day since peak corresponds to the mid-time of the spectrum. The absorbing column was fixed at 4.8
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
0.08 and 0.96
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.



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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