Rk. Prinja et al., WIND VARIABILITY OF B-SUPERGIANT .2. THE 2-COMPONENT STELLAR WIND OF GAMMA-ARAE, Astronomy and astrophysics, 318(1), 1997, pp. 157-170
The stellar wind of the rapidly rotating early-B supergiant, gamma Ara
, is studied using time series, high-resolution IUE spectroscopy secur
ed over similar to 6 days in 1993 March. Results are presented based o
n an analysis of several line species, including N V, C IV, Si IV, Si
III, C II, and Al III. Comparisons of the time-averaged wind line morp
hology of gamma Ara to the UV spectra of other OB stars, and to profil
es from spherically symmetric wind models, suggest that the wind of ga
mma Ara is equatorially enhanced. Co-existing time variable features a
re identified at low-velocity (redward of similar to 750 km s(-1)) and
at higher-speeds extending to similar to -1500 km s(-1). The observed
interface between these structures is 'defined' by the appearance of
a discrete absorption component which is extremely sharp (in velocity
space). The central velocity of this 'Super DAC' changes only graduall
y, over several days, between similar to -400 and -750 km s(-1) in mos
t of the ions. However, its location is shifted redward by almost 400
km s(-1) in Al III and C II, indicating that the physical structure gi
ving rise to this feature has a substantial velocity and ionization ju
mp. Constraints on the relative ionization properties of the wind stru
ctures are discussed. The overall wind activity in gamma Ara exhibits
a clear ion dependence, such that low-speed features are promoted in l
ow-ionization species, including Al III, C II, and Si III. We also hig
hlight that - in contrast to most OB stars - there are substantial dif
ferences in the epoch-to-epoch time-averaged wind profiles of gamma Ar
a and that the high-speed component observed during our 1993 time seri
es is normally not present. We discuss the potential roles of the radi
ative bi-stability mechanism and wind compressed regions due to rapid
stellar rotation for providing gross wind distortions in gamma Ara.