We consider a continuous sunspot data set ranging from 1853 to 1996. The em
phasis is given to long-term activity variations and north-south asymmetrie
s. The difference of the distance between sunspot belts and equator between
the northern and southern hemispheres is considered and a systematic varia
tion is found. The period of this variation is about 8.4 sunspot cycles or
about 90 years, and the amplitude is 1.3 degrees. This phenomenon could be
explained by oscillation of a quadrupolar component of solar mixed parity m
ode magnetic field.