During the unusually cold 1994-95 Arctic winter the Microwave Limb Sou
nder observed enhanced chlorine monoxide (ClO) in late Dec and through
out Feb and early Mar. Late Dec ClO was higher than during any of the
previous 3 years, consistent with the colder early winter. Between lat
e Dec 1994 and early Feb 1995, 465 K (similar to 50 hPa) vortex-averag
ed ozone (O-3) decreased by similar to 15%, with local decreases of si
milar to 30%; additional local decreases of similar to 5% were seen be
tween early Feb and early Mar. Transport calculations indicate that vo
rtex-averaged chemical loss between late Dec and early Feb was similar
to 20% at 465 K, with similar to 1/4 of that masked by downward trans
port of O-3. This Arctic chemical O-3 loss is not readily detectable i
n MLS column O-3 data.