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wave, including insights into tropical–extratropical interactions ( Fletcher and Kushner 2011 ; Garfinkel et al. 2012 ), potential connections to global warming ( Lee 2014 ), Arctic sea ice loss ( Peings and Magnusdottir 2014 ; Kim et al. 2014 ; Feldstein and Lee 2014 ), and the stratospheric polar vortex ( Limpasuvan and Hartmann 2000 ; Cohen et al. 2007 ; Garfinkel et al. 2010 ; Fletcher and Kushner 2011 ; Smith et al. 2011 ). Tropical convective forcing is known to excite a Rossby wave
wave, including insights into tropical–extratropical interactions ( Fletcher and Kushner 2011 ; Garfinkel et al. 2012 ), potential connections to global warming ( Lee 2014 ), Arctic sea ice loss ( Peings and Magnusdottir 2014 ; Kim et al. 2014 ; Feldstein and Lee 2014 ), and the stratospheric polar vortex ( Limpasuvan and Hartmann 2000 ; Cohen et al. 2007 ; Garfinkel et al. 2010 ; Fletcher and Kushner 2011 ; Smith et al. 2011 ). Tropical convective forcing is known to excite a Rossby wave
