Using new high-resolution and high signal-to-noise ratio spectroscopic obse
rvations carried out in 1992-1996, nine surface images of II Peg are obtain
ed. The inversion technique applied is the recently developed Occamian appr
oach, which does not put any artificial constraints on the solution and pro
vides an error analysis of the solution. The surface imaging is applied to
Ca I, Fe I, and Ni I lines simultaneously, a number of blending atomic and
molecular lines being included into the line list.
Two high-latitude active regions are found to dominate in all seasons, whic
h determine the spectroscopic and photometric variability. No cool polar ca
p is seen. The positions of the spots are constantly migrating to earlier o
rbital phases with approximately the same rate. This motion of the spot con
figuration means a shorter rotational period, which is just about the mean
photometric period. The mean longitude separation between the active region
s is about 180 degrees. This is considered as two active longitudes. The la
rgest of the two spots seems to be close to the central meridian, i.e. tend
s to be faced toward the secondary. In 1994 it changed its position from on
e active longitude to another, showing the effect of switching the activity
between the longitudes.