Abstract
There occurred a large stratospheric sudden warming in the southern hemisphere in late winter of 1988 which competes in suddenness and size with major mid-winter warmings in the northern hemisphere. Associated with the dynamical phenomenon of the sudden warming, total ozone increased over the eastern hemispheric part of Antarctica. The sudden warming as well as other warmings which followed it made the 1988 ozone hole shallow in depth and small in area. Long-term observation at Syowa Station (69°S, 40°E) well depict characteristics of the 1988 event.
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