Articles | Volume 20, issue 17
Atmos. Chem. Phys., 20, 10531–10544, 2020
https://doi.org/10.5194/acp-20-10531-2020
Atmos. Chem. Phys., 20, 10531–10544, 2020
https://doi.org/10.5194/acp-20-10531-2020

Research article 10 Sep 2020

Research article | 10 Sep 2020

The effect of interactive ozone chemistry on weak and strong stratospheric polar vortex events

Jessica Oehrlein et al.

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Cited articles

Albers, J. R. and Nathan, T. R.: Pathways for communicating the effects of stratospheric ozone to the polar vortex: Role of zonally asymmetric ozone, J. Atmos. Sci., 69, 785–801, 2012. a
Ayarzaguëna, B. and Serrano, E.: Monthly Characterization of the Tropospheric Circulation over the Euro-Atlantic Area in Relation with the Timing of Stratospheric Final Warmings, J. Climate, 22, 6313–6324, https://doi.org/10.1175/2009JCLI2913.1, 2009. a, b
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Baldwin, M. P. and Dunkerton, T. J.: Stratospheric Harbingers of Anomalous Weather Regimes, Science, 294, 581–584, https://doi.org/10.1126/science.1063315, 2001. a, b
Baldwin, M. P. and Thompson, D. W.: A critical comparison of stratosphere-troposphere coupling indices, Q. J. Roy. Meteor. Soc., 135, 1661–1672, 2009. a
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Winter winds in the stratosphere 10–50 km above the surface impact climate at the surface. Prior studies suggest that this interaction between the stratosphere and the surface is affected by ozone. We compare two ways of including ozone in computer simulations of climate. One method is more realistic but more expensive. We find that the method of including ozone in simulations affects the surface climate when the stratospheric winds are unusually weak but not when they are unusually strong.
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