Stratospheric ozone and aerosol distributions were measured across the
wintertime Arctic vortex from January to March 1992 with an airborne
lidar system as part of the 1992 Airborne Arctic Stratospheric Expedit
ion (AASE II). Aerosols from the Mount Pinatubo eruption were found ou
tside and inside the vortex with distinctly different distributions th
at clearly identified the dynamics of the vortex. Changes in aerosols
inside the vortex indicated advection of air from outside to inside th
e vortex below 16 kilometers. No polar stratospheric clouds were obser
ved and no evidence was found for frozen volcanic aerosols inside the
vortex. Between January and March, ozone depletion was observed inside
the vortex from 14 to 20 kilometers with a maximum average loss of ab
out 23 percent near 18 kilometers.