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Satellite Observations of the Antarctic Ozone Depletion

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Part of the book series: NATO ASI Series ((ASIC,volume 213))

Abstract

The morphology of satellite total ozone and temperature observations in the polar and subpolar Antarctic regions are reviewed. An analysis of the total ozone and 70 mb temperature data in the depletion region for for October and September shows similar secular trends. These trends result from changes which primarily occur in late September in both the minimum total ozone and temperature. The strong correlation between ozone and temperature suggests an important dynamical component to this phenomenon. A simple computation shows that a vertical velocity field of 0.06 cm/sec can account for both the secular ozone and temperature trends in the minimum region.

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References

  • Atmospheric Ozone 1985, Assessment of our Understanding of the Processes Controlling its Present Distribution and Change, 1–3, WMO Report 16, 1986.

    Google Scholar 

  • Callis, L. C., and M. Natarajan, 1986: ‘The antarctic ozone minimum: Relationship to odd chlorine, the final warming and the 11-year solar cycle,’ J Geophys. Res, 91, 10,771–10,796.

    Google Scholar 

  • Farman, J. C., B. G. Gardiner, and J. D. Schanklin, 1985: ‘Large losses of total ozone in Antarctica reveal seasonal C10x/N0x interaction,’ Nature, 315, 207–210.

    Google Scholar 

  • Farrara, J. D. and C. R. Mechoso, 1986: ‘An observational study of the final warming in the southern hemisphere stratosphere’, Geophys. Res. Lett, 13, 1232.

    Google Scholar 

  • Fleig, A. J., P. K. Bhartia, C. G. Wellemeyer, and D. S. Silberstein, 1986: ‘Sevens years of total ozone from the TOMS instrument-A Report on Data Quality’ Geophys. Res. Lett, 13, 1355–1358.

    Article  Google Scholar 

  • Geller, H. A., M. F. Wu, and H. E. Gelman, 1983: ‘Troposphere- ’Stratosphere (surface-55km) monthly winter general circulation statistics for the northern hemisphere - four year averages’ J. Atmos. Sci, 40, 1334–1352

    Article  Google Scholar 

  • Hofmann, D. J., J. H. Rosen, J. A. Harder, and S. R. Rolf, 1986: ‘Ozone and aerosol measurements in the springtime antarctic stratosphere in 1985’, Geophys. Res. Lett 13, 1252–1255.

    Article  Google Scholar 

  • Komhyr, W. D., R. D. Gross, and R. K. Leonard, 1986: ‘Total ozone decrease at South Pole, Antarctica, 1964-1985’, Geophys. Res. Lett, 13, 1248.

    Google Scholar 

  • Hahlman, J. D. and SB. Fels, 1986: ‘Antarctic ozone decreases: A dynamical cause?’ Geophys. Res. Lett., 13, 1316–1319.

    Article  Google Scholar 

  • McCormick, M. P. and J. C. Larson, 1986: ‘Antarctic springtime measurements of ozone, nitrogen dioxide and aerosol extinction by SAM II’, SAGE, and SAGE II, Geophys. Res. Lett, 13, 1280–1283.

    Google Scholar 

  • McCormick, M. P. and C. R. Trepte, 1986: ‘SAM II measurements of Antarctic PSC’s and aerosols’, Geophys. Res. Lett., 13, 1276–1279.

    Article  Google Scholar 

  • McElroy, M. B., R. J. Salawitch, S. C. Wofsy, and J. A. Logan, ‘Antarctic ozone: Reductions due to synergistic interactions in chlorine and bromine’, Nature, 321, 759–762.

    Google Scholar 

  • Newman, P. A., 1986: ‘The final warming and polar vortex disappearance during the Southern Hemisphere spring’, Geophys. Res. Lett., 13, 1228–1231

    Article  Google Scholar 

  • Newman, P. A. and H. R. Schoeberl, 1986: ‘October Antarctic temperature and total ozone trends from 1979-1985’, Geophys. Res. Lett, 13, 1206–1209.

    Article  Google Scholar 

  • Rood, R. B ., 1983: ‘Transport and the seasonal variation of ozone’, PAGEOPH, 121, 1049–1064.

    Article  Google Scholar 

  • Rosenfield, J. E., M. R. Schoeberl, and H. A. Geller, 1987: ‘A computation of the stratospheric diabatic circulation using an accurate radiative transfer model’, Atmos. Sci, 44, 859–876.

    Google Scholar 

  • Schoeberl, M. R., A. J. Krueger, and P. A. Newman, ‘The morphology of Antarctic total ozone as seen by TOMS’,Geophys. Res. Lett, 13, 1217–1220, 1986.

    Article  Google Scholar 

  • Solomon, S., R. R. Garcia, F. S. Rowland, and D. Wuebbles, 1986: ‘On the depletion of Antarctic ozone’, Nature, 321, 755–758.

    Google Scholar 

  • Stolarski, R. S. and M. R. Schoeberl, 1986: ‘Further interpretation of satellite measurements of Antarctic total ozone’, Geophys. Res. Lett, 13, 1210–1212

    Article  Google Scholar 

  • Tung, K. K., M. K. W. Ko, J. M. Rodriguez, and N. D. Sze, 1986: ‘Are Antarctic ozone variations a manifestation of dynamics or chemistry’, Nature, 322, 8811–8813.

    Article  Google Scholar 

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© 1987 D. Reidel Publishing Company, Dordrecht, Holand.

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Schoeberl, M.R. (1987). Satellite Observations of the Antarctic Ozone Depletion. In: Visconti, G., Garcia, R. (eds) Transport Processes in the Middle Atmosphere. NATO ASI Series, vol 213. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-3973-8_11

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  • DOI: https://doi.org/10.1007/978-94-009-3973-8_11

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-8262-4

  • Online ISBN: 978-94-009-3973-8

  • eBook Packages: Springer Book Archive

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