Atmos. Chem. Phys. Discuss., 13, 12337-12387, 2013
www.atmos-chem-phys-discuss.net/13/12337/2013/
doi:10.5194/acpd-13-12337-2013
© Author(s) 2013. 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.
Trends in stratospheric ozone profiles using functional mixed models
A. Y. Park1, S. Guillas1, and I. Petropavlovskikh2
1Department of Statistical Science, University College London, London, UK
2CIRES, University of Colorado, Boulder, Colorado, USA

Abstract. This paper is devoted to the modeling of altitude-dependent patterns of ozone variations over time. Umkher ozone profiles (quarter of Umkehr layer) from 1978 to 2011 are investigated at two locations: Boulder (USA) and Arosa (Switzerland). The study consists of two statistical stages. First we approximate ozone profiles employing an appropriate basis. To capture primary modes of ozone variations without losing essential information, a functional principal component analysis is performed as it penalizes roughness of the function and smooths excessive variations in the shape of the ozone profiles. As a result, data driven basis functions are obtained. Secondly we estimate the effects of covariates – month, year (trend), quasi biennial oscillation, the Solar cycle, arctic oscillation and the El Niño/Southern Oscillation cycle – on the principal component scores of ozone profiles over time using generalized additive models. The effects are smooth functions of the covariates, and are represented by knot-based regression cubic splines. Finally we employ generalized additive mixed effects models incorporating a more complex error structure that reflects the observed seasonality in the data. The analysis provides more accurate estimates of influences and trends, together with enhanced uncertainty quantification. We are able to capture fine variations in the time evolution of the profiles such as the semi-annual oscillation. We conclude by showing the trends by altitude over Boulder. The strongly declining trends over 2003–2011 for altitudes of 32–64 hPa show that stratospheric ozone is not yet fully recovering.

Citation: Park, A. Y., Guillas, S., and Petropavlovskikh, I.: Trends in stratospheric ozone profiles using functional mixed models, Atmos. Chem. Phys. Discuss., 13, 12337-12387, doi:10.5194/acpd-13-12337-2013, 2013.
 
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