A comparison of sensitivity in extratropical circulation in the Northern Hemisphere (NH) and Southern Hemisphere (SH) is conducted through observational analyses and diagnostic linear model experiments for two types of El Ni?o events, the traditional El Ni?o with the strongest warmth in the eastern tropical Pacific (EP El Ni?o) and the El Ni?o Modoki with the strongest warmth in the central tropical Pacific (CP El Ni?o). It is shown that CP El Ni?o favors the occurrence of a negative-phase Northern Annular Mode (NAM), while EP El Ni?o favors that of the Pacific-North American (PNA) pattern. In SH, both EP and CP El Ni?o induce a negative phase Southern Annular Mode (SAM). However, the former has a greater amplitude, which is consistent with the stronger sea surface temperature (SST) warmth. The difference in the two types of El Ni?o events in NH may originate from the dependence of heating-induced extratropical response on the location of initial heating, which may be associated with activity of the stationary wave. In SH, the lack of sensitivity to the location of heating can be associated with weaker activity of the stationary wave therein.