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Hailan Wang, Siegfried Schubert, Randal Koster, Yoo-Geun Ham, and Max Suarez

Feng 2012 ; Dai 2013 ) and atmospheric general circulation model (AGCM) simulations (e.g., Hoerling and Kumar 2003 ; Schubert et al. 2004a , b ; Seager et al. 2005 ; Wang et al. 2010 ). An important finding from such studies is that ENSO and the PDO in their cold phases, and the AMO in its warm phase, produce a tendency for drought conditions over the United States, with the Pacific playing the dominant role (e.g., Mo et al. 2009 ; Schubert et al. 2009 ). In addition, the impact of SST

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