Contrasting Impacts of Two Types of ENSO on the Boreal Spring Hadley Circulation

The possible influences of two types of ENSO [i.e., the canonical ENSO and ENSO Modoki (EM)] on Hadley circulation (HC) during the boreal spring are investigated during 1979‐2010. El Ni~ no events are featured with a symmetric pattern in equatorial zonal-mean sea surface temperature anomalies (SSTA), with a maximum around the equator. In contrast, the zonal-mean SSTA associated with El Ni~ Modoki events shows an asymmetric structure with a maximum around 108N. The contrasting underlying thermal structures corresponding with ENSO and EM have opposite impacts on the simultaneous HC. In El Ni~ years, a symmetric anomalous meridional circulation is seen, with enhanced rising around the equator and anomalousdescentatabout158Nand208S.Incontrast,anasymmetricequatorialmeridionalcirculationisobserved for El Ni~ Modoki years, with anomalous ascent around 108N and descent at about 108S and 208N. The contrasting meridional circulation anomalies within ENSO and EM are caused by their different meridional SSTA structure. This result is theoretically explained, indicating that anomalous meridional circulation is subject to the meridional SSTA gradient. Moreover, the observed results are reproduced in numerical experiments driven by anomalous warming in the eastern and central Pacific Ocean. Thus, the authors conclude that the anomalous HC linked to ENSO and EM is induced by the accompanying meridional gradient in zonal-mean SSTA.