A. Parrish et al., MICROWAVE OZONE AND LIDAR AEROSOL PROFILE OBSERVATIONS AT TABLE-MOUNTAIN, CALIFORNIA, FOLLOWING THE PINATUBO ERUPTION, J GEO RES-A, 103(D17), 1998, pp. 22201-22208
Ozone profiles measured with a ground-based microwave instrument in ye
ars from 1989 through 1992 at latitude 34 degrees N. were searched for
effects arising from the eruption of Mount Pinatubo in 1991. Between
20 and 24 km, ozone values after November 1991 were systematically les
s than in earlier years, and the deviation generally grew with time th
rough May 1992, The minimum was 11 to 15% below values in earlier year
s, and occurred later than minima observed with ozonesondes at higher
latitudes or predicted by some models. Although there was a steady inc
rease in ozone levels in the 18-10 hPa range between February and May
1992, the highest values were not significantly above normal. Effects
of the quasi-biennial oscillation on ozone values are much smaller tha
n the observed changes. Colocated lidar observations show that stratos
pheric aerosol levels were steadily elevated from November 1991 throug
h at least March 1992, with some intermittent activity in late August
through October 1991. The main aerosol cloud thus arrived at the same
time as depletion first appeared.