Abstract

We reanalyse archival GINGA and ASCA X-ray data from SS Cyg in both quiescence and outburst, using multi-temperature plasma models for the continuum and line emission, together with their reflection from the X-ray illuminated white dwarf and accretion disk. Reflection is clearly detected in all the spectra, but its contribution is larger in the softer X-ray spectra seen in outburst than in quiescence. This supports models in which the quiescent inner disk is not present or not optically thick, so that the only reflector is the white dwarf surface rather than the white dwarf plus the disk. We detect partially ionized absorption in the ASCA outburst spectrum, which is probably the X-ray signature of the outflowing wind. The ASCA data also allow a detailed measure of the elemental abundances. We find that all detectable lines from the hot plasma (except perhaps Si and S) are a factor $\sim 2.5\times$ weaker than expected from solar abundances. We examine possible deviations from coronal equilibrium, but conclude that the heavy elements are truly underabundant in SS Cyg. In quiescence the underlying intrinsic spectrum is consistent with a single temperature plasma. This conflicts with the expected cooling of the material, and requires that either the plasma is reheated or that the cooler emission is masked by absorption in an optically thin inner disk which affects only that part of the boundary layer emission below the disk. By contrast, the outburst spectrum is much softer and is dominated by the cooling components but has a total hot plasma luminosity similar to that in quiescence, showing that the optically thin plasma emission is important even in outburst.

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