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John R. Albers, John P. McCormack and Terrence R. Nathan Stratospheric ozone and the morphology of the northern hemisphere planetary waveguide Journal of Geophysical Research: Atmospheres 118

Article first published online: 31 JAN 2013 | DOI: 10.1029/2012JD017937

Key Points

  • Ozone changes the meridional and vertical extent of the planetary waveguide
  • Ozone increases the wave activity flux from the lower into the upper
  • Ozone causes a warmer and weaker stratospheric polar vortex

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