The Microwave Limb Sounder (MLS) observed ozone (O-3) loss in the Arct
ic vortex beginning in January 1997 at 585 K (similar to 25 hPa) and i
n February 1997 at 465 K (similar to 50 hPa). Minimum vortex-averaged
O-3 mixing ratios observed in 1997 were higher than those in 1996, whi
ch were the lowest ever recorded by MLS. The vertical extent of O-3 lo
ss and maximum local O-3 decreases were larger, but the decrease fille
d the vortex less completely, in 1997 than in 1996. Unusually low high
-latitude column O-3 above 100 hPa in April 1997 resulted mainly from
dynamical effects of the unusually persistent lower stratospheric vort
ex and winter-like temperature patterns. Column O-3 above 100 hPa aver
aged in comparable regions of the vortex showed a stronger decreasing
trend in 1996-97 than in 1995-96, consistent with the larger vertical
extent and maximum local values of lower stratospheric O-3 loss. Chemi
cal O-3 loss resulted in an similar to 10% observed decrease in column
O-3 between late January and early April 1997.