We present spectroscopic and timing analyses of the hot DA white dwarf GD 3
94 showing abundance inhomogeneities across its surface. Lick Hamilton eche
lle, International Ultraviolet Explorer (IUE), HST GHRS, and Hopkins Ultrav
iolet Telescope (HUT) spectra show dominant Si III and Si IV features, whil
e Extreme Ultraviolet Explorer (EUVE) spectra show evidence of a host of tr
ace element opacities. We report the detection of Si III lambda 4552 triple
t with a measured radial velocity of 27 km s(-1) in agreement with far ultr
aviolet (FUV) line velocities, but indicating a silicon abundance (Si/H = 2
x 10(-5)) a factor of 10 larger than measured in the FUV range [Si/H = (2-
7) x 10(-6)]. Effective temperature measurements based on Lyman continuum (
EUVE) and Lyman line series (HUT) are systematically cooler (Delta T simila
r to -4000 K) than measurements based on medium-dispersion Balmer line spec
troscopy, an effect attributed to yet unidentified opacities. A timing anal
ysis of EUVE: deep-survey and scanner time series, as well as spectrometer
data, shows GD 394 to be variable in the extreme ultraviolet (EUV) with an
amplitude of 25% and a period of 1.150 +/- 0.003 days. The EUV variability
suggests abundance inhomogeneities in the atmosphere, and we explore differ
ent models to explain its origin.