Variations of tropospheric ozone concentration over Syowa Station, Antarctica
Aircraft measurements of the tropospheric O 3 concentration were made over Syowa Station (69°00'S, 39°35'E), Antarctica from May 1989 to January 1990, except during the polar night months of June and July. The O 3 concentration increased with height for the whole period of the measurements...
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Veröffentlicht in: | Tellus. Series B, Chemical and physical meteorology Chemical and physical meteorology, 1992-01, Vol.44 (4), p.262-272 |
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Sprache: | eng |
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Zusammenfassung: | Aircraft measurements of the tropospheric O
3
concentration were made over Syowa Station (69°00'S, 39°35'E), Antarctica from May 1989 to January 1990, except during the polar night months of June and July. The O
3
concentration increased with height for the whole period of the measurements. Lower tropospheric O
3
showed a prominent seasonal variation with maximum concentration in winter and minimum concentration in summer, which is very close to the result of continuous O
3
measurements initiated at Syowa Station in February 1988. In the upper troposphere, the concentration reached high values in winter, decreased gradually until late spring and then increased again. As a result, the height-dependent difference of the concentration was reduced from late autumn to early spring and enhanced in remaining seasons of the year. The seasonal variation of upper tropospheric O
3
was similar to those of the lower stratospheric O
3
concentration measured by ozonesondes and the total amount of O
3
by a Dobson spectrophotometer over Syowa Station. Inspection of TOMS (Total Ozone Mapping Spectrometer) data also suggested that the temporal variations of the upper tropospheric O
3
measured in this study are closely related to those of the lower stratospheric O
3
over Syowa Station. Comparison of the results of surface O
3
measurements in the southern hemisphere showed that the concentration increase going southward, and appearance of the minimum concentration of the seasonal variation is delayed by almost 1 month at the South Pole compared to Syowa Station and Cape Grim, Tasmania. Taking into account these results, it is suggested that the intrusion of stratospheric O
3
into the troposphere occurs over Syowa Station throughout the year, and that air with low O
3
concentrations is transported from subpolar or middle latitudes to the station through the lower troposphere from spring to early autumn, in addition to the photochemical destruction of O
3
near the station. |
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ISSN: | 0280-6509 1600-0889 |
DOI: | 10.3402/tellusb.v44i4.15454 |