Sm. Hollandsworth et al., OZONE TRENDS DEDUCED FROM COMBINED NIMBUS-7 SBUV AND NOAA-11 SBUV 2 DATA/, Geophysical research letters, 22(8), 1995, pp. 905-908
The long-term time series of global ozone from the Nimbus-7 SBUV (Nov.
1978-June 1990) are extended through June 1994 by using measurements
from the NOAA-11 SBUV/2. The data sets are merged based upon compariso
ns during the 18-month overlap period in which both instruments were o
perational. During this period, the average offset between the two tim
e series is less than 2% in total ozone, and less than 6% in Umkehr la
yers 1-10. A linear-regression trend model is applied to the extended
time series to calculate updated trends as a function of latitude and
altitude. Trends through June 1994 are 1.5-2% per decade less negative
than through June 1990 in the tropical middle stratosphere (35-40 km)
and in the upper stratosphere (45-50 km) at mid-latitudes. In the low
er stratosphere, the trends are nearly 15% per decade more negative in
the southern hemisphere tropical regions to 25 degrees S, but remain
relatively unchanged elsewhere. The seasonal structure of the total oz
one trends is similar to past trend study results, but the magnitude o
f the seasonal trend can vary by 2% per decade depending on the length
of the time series. Both TOMS (through April 1993) and SBUV total ozo
ne time series show small negative trends in the equatorial region, th
ough they are not statistically significant at the 2-sigma level.