Articles | Volume 15, issue 9
Atmos. Chem. Phys., 15, 4997–5005, 2015
https://doi.org/10.5194/acp-15-4997-2015
Atmos. Chem. Phys., 15, 4997–5005, 2015
https://doi.org/10.5194/acp-15-4997-2015
Research article
04 May 2015
Research article | 04 May 2015

Observations of planetary waves in the mesosphere-lower thermosphere during stratospheric warming events

N. H. Stray et al.

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Cited articles

Chandran, A., Collins, R. L., Garcia, R. R., Marsh, D. R., Harvey, V. L., Yue, J., and de la Torre, L.: A climatology of elevated stratopause events in the whole atmosphere community climate model, J. Geophys. Res., 118, 1234–1246, https://doi.org/10.1002/jgrd.50123, 2013a.
Chandran, A., Garcia, R. R., Collins, R. L., and Chang, L. C.: Secondary waves in the middle and upper atmosphere following the stratospheric sudden warming event of january 2012, Geophys. Res. Lett., 40, 1–7, https://doi.org/10.1002/grl.50373, 2013b.
Chandran, A., Collins, R., and Harvey, V.: Stratosphere-mesosphere coupling during stratospheric sudden warming events, Adv. Space Res., 53, 1265–1289, https://doi.org/10.1016/j.asr.2014.02.005, 2014.
de Wit, R. J., Hibbins, R. E., Espy, P. J., Orsolini, Y. J., Limpasuvan, V., and Kinnison, D. E.: Observations of gravity wave forcing of the mesopause region during the january 2013 major sudden stratospheric warming, Geophys. Res. Lett., 41, 4745–4752, https://doi.org/10.1002/2014GL060501, 2014.
Eyring, V., Shepherd, T. G., and Waugh, D. W. (Eds.): SPARC CCMVal Report on the Evaluation of Chemistry-Climate Models, V., SPARC Report No. 5, WCRP-X, WMO/TD-No.X, available at: http://www.sparc-climate.org/publications/sparc-reports/sparc-report-no5/ (last access: 30 April 2015), 2010.
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Short summary
Planetary wave activity measured in the mesosphere to lower thermosphere is shown to increase drastically after strong stratospheric polar cap wind reversals associated with sudden stratospheric warmings. In addition, a moderate but significant correlation was found between planetary wave enhancement in the mesosphere to lower thermosphere and all stratospheric polar cap wind reversals, irrespective of the strength of the reversal.
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