Gerber, Edwin P.Butler, AmyCalvo Fernández, NataliaCharlton-Perez, AndrewGiorgetta, MarcoManzini, ElisaPerlwitz, JudithPolvani, Lorenzo M.Sassi, FabrizioScaife, Adam A.Shaw, Tiffany A.Son, Seok-WooWatanabe, Shingo2023-06-202023-06-202012-060003-000710.1175/BAMS-D-11-00145.1https://hdl.handle.net/20.500.14352/44182© 2012 American Meteorological Society. We thank Dr. Ben Ruston of the Marine Meteorology Division of the Naval Research Laboratory for permission to use the data in Fig. 2, and two anonymous reviewers for their comments on an earlier draft of the manuscript. EPG gratefully acknowledges the support of the National Science Foundation through the Atmospheric and Geospace Sciences program. FS acknowledges the support of the Office of Naval Research through NRL's base 6.1 and 6.2 research programs. JP's contribution is supported by NOAA's Climate Program Office, and MG and EM acknowledge the partial support of the COMBINE project of the European Commission's Seventh Framework Programme.New modeling efforts will provide unprecedented opportunities to harness our knowledge of the stratosphere to improve weather and climate prediction.engjournal articlehttp://dx.doi.org/10.1175/BAMS-D-11-00145.1http://journals.ametsoc.org/open access52Quasi-biennial oscillationRelatively simple AGCMPolar ozone depletionNorthern-hemisphereClimate-ChangeTropospheric circulationArctic oscillationSurface weatherSimplified GCMAnnular modesAstrofísicaAstronomía (Física)Física atmosférica2501 Ciencias de la Atmósfera