Rs. Stolarski et al., SPRINGTIME ANTARCTIC TOTAL OZONE MEASUREMENTS IN THE EARLY-1970S FROMTHE BUV INSTRUMENT ON NIMBUS-4, Geophysical research letters, 24(5), 1997, pp. 591-594
Data from the BUV instrument on the Nimbus 4 satellite have been used
to construct maps of the measured total ozone field over the Antarctic
region during the Austral springs of 1970 through 1973. These maps sh
ow an October mean ozone distribution similar to that measured in 1979
by the Nimbus 7 TOMS instrument. These ozone maps during the 1970s ar
e very different from those measured during the late 1980s and early 1
990s. The ozone distribution for each of the years during the early 19
70s is characterized by a circumpolar, crescent-shaped maximum surroun
ding a shallow minimum centered near the pole. The total ozone amounts
in the polar minimum region in the early 1970s average about 300 Dobs
on units, comparable to the amounts measured at that time over Halley
Bay and Syowa by ground-based Dobson Spectrophotometers.