The browser you are using is not supported by this website. All versions of Internet Explorer are no longer supported, either by us or Microsoft (read more here: https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Please use a modern browser to fully experience our website, such as the newest versions of Edge, Chrome, Firefox or Safari etc.

Default user image.

Markku Rummukainen

Professor

Default user image.

Depletion of column ozone in the arctic during the winters of 1993-94 and 1994-95

Author

  • F. Goutail
  • J. P. Pommereau
  • C. Phillips
  • C. Deniel
  • A. Sarkissian
  • F. Lefèvre
  • E. Kyro
  • M. Rummukainen
  • P. Ericksen
  • S. B. Andersen
  • B. A. Kaastad-Hoiskar
  • G. Braathen
  • V. Dorokhov
  • V. U. Khattatov

Summary, in English

The total ozone reduction in the Arctic during the winters of 1993/94 acid 1994/95 has been evaluated using the ground-based total ozone measurements of five SAOZ spectrometers distributed in the Arctic and from number density profiles of a balloon-borne version of the instrument. The ozone change resulting from transport has been removed using a 3D Chemistry Transport Model (CTM) run without chemistry. A cumulative total ozone depletion at the end of winter in March of 18% ± 4% in 1994 and of 32% ± 4% in 1995 was observed within the polar vortex, and of 15% ± 4% in both years outside the vortex. This evaluation is not sensitive to the vertical transport in the model. The periods, locations and altitudes at which ozone loss occurred were tightly connected to temperatures lower than NAT condensation temperature. The maximum loss was observed at 50 hPa in 1994 and lower, 60-80 hPa, in 1995. Half of the depletion in 1994 and three quarters in 1995 occurred during the early winter, showing that a late final warming is not a prerequisite for large ozone destruction in the northern hemisphere. The timing, the geographical location and the altitude of the ozone losses are well captured by the 3D CTM photochemical model using current chemistry, but its amplitude at low sun during the early winter, is underestimated. The model simulations also capture the early season reductions observed outside the vortex. This suggests that the losses occurred in situ in the early winter, when low temperatures are frequent, and not later in March, when ozone is most reduced inside the vortex, which would be the case if leakage from the vortex was the cause of the depletion.

Publishing year

1999

Language

English

Pages

1-34

Publication/Series

Journal of Atmospheric Chemistry

Volume

32

Document type

Journal article

Publisher

Springer

Keywords

  • Balloon-sonde
  • Ground-based
  • Model
  • Ozone loss
  • Stratosphere

Status

Published

ISBN/ISSN/Other

  • ISSN: 0167-7764