From 1971 through April 1997 we have tracked the variation of stratosp
heric HCl using ground-based spectroscopic observations of the sun. Th
is HCl is a tracer of free chlorine, the agent which catalytically des
troys ozone. Our observations are dominated by a general increase in H
Cl by a factor between three and four, although since about 1990 the r
ate of increase may have slowed.