  We present measurements of the effective temperatures and surface gravities
for a sample of hot DA white dwarfs, using the Lyman line data available from
the HUT, ORFEUS and FUSE far-UV space missions. Comparing the results with
those from the standard Balmer line technique, we find that there is a general
good overall agreement between the two methods. However, significant
differences are found for a number of stars, but not always of a consistent
nature in that sometimes the Balmer temperature exceeds that derived from the
Lyman lines and in other instances is lower. We conclude that, with the latest
model atmosphere calculations, these discrepancies probably do not arise from
an inadequate theoretical treatment of the Lyman lines but rather from
systematic effects in the observation and data reduction processes, which
dominate the statistical errors in these spectra. If these systematic data
reduction effects can be adequately controlled, the Lyman line temperature and
gravity measurements are consistent with those obtained from the Balmer lines
when allowance is made for reasonable observational uncertainties.
