Solar wind composition provides a strong source of variability for cometary
X-rays. Using recently constrained composition observations from the Solar
Wind Ion Composition Spectrometer on the Ulysses spacecraft (SWICS/Ulysses
) and information on ion-neutral charge-transfer collisions, we model comet
ary X-ray emission and its variability. Fast and slow solar wind cases are
adopted and compared to observations of X-ray spectra from the Rontgen-Sate
llit (ROSAT) for comet Levy. The predicted and observed spectra compare mos
t favorably for fast solar wind in optically thin conditions. Solar wind co
mposition can be predicted as a function of the coronal temperature near it
s source and, consequently, cometary X-ray spectra may be predicted as a fu
nction of the solar wind's coronal temperature. Implications and additional
developments necessary to unravel the compositional information contained
in X-ray spectra are explored.