Atmos. Chem. Phys. Discuss., 11, 13829-13865, 2011
www.atmos-chem-phys-discuss.net/11/13829/2011/
doi:10.5194/acpd-11-13829-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
The Brewer-Dobson circulation and total ozone from seasonal to decadal time scales
M. Weber1, S. Dikty1, J. P. Burrows1, H. Garny2, M. Dameris2, A. Kubin3, J. Abalichin3, and U. Langematz3
1Institut für Umweltphysik, Universität Bremen FB1, Bremen, Germany
2Institut für Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt e.V., Oberpfaffenhofen, Germany
3Institut für Meteorologie, Freie Universität Berlin, Berlin, Germany

Abstract. The effect of the winter Brewer-Dobson circulation (BDC) on the seasonal and decadal evolution of total ozone in both hemispheres is investigated using satellite total ozone data and outputs from two chemistry-climate models (CCM). Combining data from both hemispheres a linear relationship between the winter cumulative extratropical 100 hPa eddy heat flux and the ozone ratio with respect to fall ozone levels exists and is statistically significant for tropical as well as polar ozone. The high correlation at high latitudes persists well into the summer months until the onset of the next winter season. The anti-correlation of the cumulative eddy heat flux with tropical ozone ratios, however, breaks down in spring as the polar vortex erodes and changes to a weak positive correlation similar to that observed at high latitudes. The inter-annual variability and decadal evolution of ozone in each hemisphere in winter, spring, and summer are therefore driven by the cumulative effect of the previous winter's meridional circulation. This compact linear relationship is also found in two different CCMs (EMAC-FUB, DLR-E39C-A) indicating that current models realistically describe the variability in stratospheric circulation and its climate effect on total ozone. Both models show a positive trend in the winter mean eddy heat flux (and winter BDC strength) in both hemispheres until year 2050, however the inter-annual variability (peak-to-peak) is two to three times larger than the mean change between 1960 and 2050. It is, therefore, possible to detect a shift in this compact linear relationship related to past and future changes in the stratospheric halogen load. A similar shift is difficult to derive from observational data since the satellite era now spanning more than thirty years is still fairly short.

Citation: Weber, M., Dikty, S., Burrows, J. P., Garny, H., Dameris, M., Kubin, A., Abalichin, J., and Langematz, U.: The Brewer-Dobson circulation and total ozone from seasonal to decadal time scales, Atmos. Chem. Phys. Discuss., 11, 13829-13865, doi:10.5194/acpd-11-13829-2011, 2011.
 
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