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prolong period of time) in the United States on seasonal time scales mainly result from sea surface temperature (SST) anomalies in the Pacific associated with El Niño–Southern Oscillation (ENSO) and/or the Pacific decadal oscillation (PDO), with lesser contribution from SST anomalies in the Atlantic and Indian Oceans (e.g., Hoerling and Kumar 2003 ; McCabe et al. 2004 ; Seager et al. 2005 ; Cook et al. 2007 ; Hoerling et al. 2009 ; Seager and Hoerling 2014 ; Schubert et al. 2016 ; Huang et al
prolong period of time) in the United States on seasonal time scales mainly result from sea surface temperature (SST) anomalies in the Pacific associated with El Niño–Southern Oscillation (ENSO) and/or the Pacific decadal oscillation (PDO), with lesser contribution from SST anomalies in the Atlantic and Indian Oceans (e.g., Hoerling and Kumar 2003 ; McCabe et al. 2004 ; Seager et al. 2005 ; Cook et al. 2007 ; Hoerling et al. 2009 ; Seager and Hoerling 2014 ; Schubert et al. 2016 ; Huang et al
