The last two winter-spring seasons (DJFM) distinguished themselves by
being with the lowest ever total ozone over all three continental size
regions between 45-degrees-N and 65-degrees-N of North America, Europ
e and Siberia. The total ozone deficiencies for the entire season over
all of the above mentioned regions were about 11% and 13% below the l
ong-term normal during the two consecutive years (1991/92 and 1992/93
respectively). This helped to pull down the cumulative ozone decline s
ince the winter-spring of 1969/70 to be about 14% in the latitude belt
of the 45-degrees-N- 65-degrees-N. Frequencies of days with ozone val
ues deviating below the long-term mean by more than 2sigma have been t
en times higher than their 35-year average. There are evidences deduce
d from trajectories on potential temperature surfaces that transport o
f poor in ozone air masses forced in addition by vertical motions, cou
ld account for a number of the extreme cases. There is also evidence t
hat cold air, known to have excess ClO content, has moved over the sun
lighted latitudes on many occasions, when chemical ozone destruction
could have been favored. These ozone deficiencies do not have similar
rates of decline and did not reach even close to the extreme low value
s regularly observed during the Antarctic-spring ozone hole phenomena.