We present ASCA observations of the dwarf nova Z Camelopardalis during outb
urst and during a transition from quiescence to another outburst.
At the beginning of the transition the X-ray count rate was an order of mag
nitude higher and the spectrum much harder than during the outburst. As the
transition progressed, the spectrum remained hard as the X-ray flux decrea
sed by a factor of 3, with no spectral softening.
Spectral modelling reveals an optically thin, high-temperature component (k
T approximate to 10 keV) which dominates the transition observation and is
also observed during outburst. This is expected from material accreting on
to the white dwarf surface. The outburst spectra require additional emissio
n at lower temperatures, through either an additional discrete temperature
component, or a combination of a cooling flow model and an ionized absorber
.
Fits to both observations show large amounts of absorption (N-H = 8-9 X 10(
21) cm(-2)), two orders of magnitude greater than the measured interstellar
value, and consistent with UV measurements of the outburst. This suggests
that a disc wind is present even in the earliest stages of outburst, possib
ly before the outburst heating wave has reached the boundary layer.