Articles | Volume 19, issue 10
Atmos. Chem. Phys., 19, 6659–6679, 2019
https://doi.org/10.5194/acp-19-6659-2019

Special issue: The SPARC Reanalysis Intercomparison Project (S-RIP) (ACP/ESSD...

Atmos. Chem. Phys., 19, 6659–6679, 2019
https://doi.org/10.5194/acp-19-6659-2019

Research article 20 May 2019

Research article | 20 May 2019

Variability of temperature and ozone in the upper troposphere and lower stratosphere from multi-satellite observations and reanalysis data

Ming Shangguan et al.

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Cited articles

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Bandoro, J., Solomon, S., Santer, B. D., Kinnison, D. E., and Mills, M. J.: Detectability of the impacts of ozone-depleting substances and greenhouse gases upon stratospheric ozone accounting for nonlinearities in historical forcings, Atmos. Chem. Phys., 18, 143–166, https://doi.org/10.5194/acp-18-143-2018, 2018. a
Chipperfield, M. P., Dhomse, S., Hossaini, R., W., F., Santee, M., Weber, M., Burrows, J. P., Wild, J., Loyola, D., and Coldewey-Egbers, M.: On the Cause of Recent Variations in Lower Stratospheric Ozone, Geophys. Res. Lett., 45, 1–9, 2018. a, b, c, d
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Short summary
A significant warming in the troposphere and cooling in the stratosphere are found in satellite measurements (2002–2017). The newest ERA5 data are first used for analyzing temperature and ozone trends in the UTLS and show the best quality compared to other reanalyses. According to model simulations, the temperature increase in the troposphere and ozone decrease in the NH stratosphere are mainly connected to a surface warming of the ocean and subsequent changes in atmospheric circulation.
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