Articles | Volume 10, issue 7
Geosci. Model Dev., 10, 2671–2689, 2017
https://doi.org/10.5194/gmd-10-2671-2017
Geosci. Model Dev., 10, 2671–2689, 2017
https://doi.org/10.5194/gmd-10-2671-2017

Model description paper 13 Jul 2017

Model description paper | 13 Jul 2017

Update of the Polar SWIFT model for polar stratospheric ozone loss (Polar SWIFT version 2)

Ingo Wohltmann et al.

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Cited articles

Cariolle, D. and Déqué, M.: Southern hemisphere medium-scale waves and total ozone disturbances in a spectral general circulation model, J. Geophys. Res., 91, 10825–10846, 1986.
Cariolle, D. and Teyssèdre, H.: A revised linear ozone photochemistry parameterization for use in transport and general circulation models: multi-annual simulations, Atmos. Chem. Phys., 7, 2183–2196, https://doi.org/10.5194/acp-7-2183-2007, 2007.
Cariolle, D., Lasserre-Bigorry, A., Royer, J.-F., and Geleyn, J.-F.: A general circulation model simulation of the springtime Antarctic ozone decrease and its impact on mid-latitudes, J. Geophys. Res., 95, 1883–1898, 1990.
Eyring, V., Shepherd, T. G., and Waugh, D. W.: SPARC CCMVal Report on the Evaluation of Chemistry-Climate Models, SPARC Report No. 5, http://www.sparc-climate.org/publications/sparc-reports/ (last access: 4 July 2017), 2010.
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Short summary
The Polar SWIFT model is a fast scheme for calculating the chemistry of stratospheric ozone depletion in polar winter. It is intended for use in global climate models (GCMs) and Earth system models (ESMs) to enable the simulation of mutual interactions between the ozone layer and climate.