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Michael S. Pritchard, Andrew B. G. Bush, and Shawn J. Marshall

associated with the propagation of atmospheric planetary waves excited during El Niño, which may give rise to the Pacific–North American (PNA) pattern ( Straus and Shukla 2002 ). Recent studies on the dynamics of ENSO teleconnections have investigated the effects of transient eddies, diabatic cooling processes ( DeWeaver and Nigam 2004 ; Trenberth et al. 2002 ), and sources of nonlinear ENSO variability (e.g., Hannachi 2001 ; Wu and Hsieh 2004 ), all of which likely contribute to the development of

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