Articles | Volume 19, issue 7
Atmos. Chem. Phys., 19, 4289–4309, 2019
https://doi.org/10.5194/acp-19-4289-2019
Atmos. Chem. Phys., 19, 4289–4309, 2019
https://doi.org/10.5194/acp-19-4289-2019

Research article 03 Apr 2019

Research article | 03 Apr 2019

Ground-based ozone profiles over central Europe: incorporating anomalous observations into the analysis of stratospheric ozone trends

Leonie Bernet et al.

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Cited articles

Bai, K., Chang, N.-B., Shi, R., Yu, H., and Gao, W.: An inter-comparison of multi-decadal observational and reanalysis data sets for global total ozone trends and variability analysis, J. Geophys. Res.-Atmos., 122, 1–21, https://doi.org/10.1002/2016JD025835, 2017. a
Ball, W. T., Alsing, J., Mortlock, D. J., Rozanov, E. V., Tummon, F., and Haigh, J. D.: Reconciling differences in stratospheric ozone composites, Atmos. Chem. Phys., 17, 12269–12302, https://doi.org/10.5194/acp-17-12269-2017, 2017. a, b, c
Ball, W. T., Alsing, J., Mortlock, D. J., Staehelin, J., Haigh, J. D., Peter, T., Tummon, F., Stübi, R., Stenke, A., Anderson, J., Bourassa, A., Davis, S. M., Degenstein, D., Frith, S. M., Froidevaux, L., Roth, C., Sofieva, V., Wang, R., Wild, J., Yu, P., Ziemke, J. R., and Rozanov, E. V.: Evidence for continuous decline in lower stratospheric ozone offsetting ozone layer recovery, Atmos. Chem. Phys., 18, 1379–1394, https://doi.org/10.5194/acp-18-1379-2018, 2018. a, b
Bates, B. C., Chandler, R. E., and Bowman, A. W.: Trend estimation and change point detection in individual climatic series using flexible regression methods, J. Geophys. Res.-Atmos., 117, 1–9, https://doi.org/10.1029/2011JD017077, 2012. a
Bourassa, A. E., Roth, C. Z., Zawada, D. J., Rieger, L. A., McLinden, C. A., and Degenstein, D. A.: Drift-corrected Odin-OSIRIS ozone product: Algorithm and updated stratospheric ozone trends, Atmos. Meas. Tech., 11, 489–498, https://doi.org/10.5194/amt-11-489-2018, 2018. a
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Short summary
After severe ozone depletion, upper stratospheric ozone has started to recover in recent years. However, stratospheric ozone trends from various data sets still show differences. To partly explain such differences, we investigate how the trends are affected by different factors, for example, anomalies in the data. We show how trend estimates can be improved by considering such anomalies and present updated stratospheric ozone trends from ground data measured in central Europe.
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