Microwave Limb Sounder (MLS) measurements of lower stratospheric ClO a
nd gas-phase HNO3 are presented for the 1996-97 Arctic winter. The hor
izontal and vertical extent of enhanced ClO were smaller in 1997 than
in 1996, as was the degree of enhancement. This is consistent with dif
ferences in the evolution and vertical structure of temperatures in th
e two years. Gas-phase HNO3 abundances, which increased in early winte
r due to diabatic descent, exhibited a decreasing trend from mid to la
te winter in all six Arctic winters observed by MLS, probably due to i
ncreasing HNO3 photolysis throughout this period.