Why did the 2015/16 El Niño Fail to Bring Excessive Precipitation to California?

California has experienced severe drought in recent years posing great challenges to water resources, agriculture, and land management. El Niño, as the prime sources of seasonal to interannual climate predictability, offers the potential of alleviation of drought in California. Here, El Niño's impacts on California winter precipitation are examined. Our results, based on the observations during 1901-2010, show that El Niño's influence on precipitation strengthens from early to late winter even as El Niño weakens. The cause of the nonlinear relationship between sea surface temperature anomaly (SSTA) amplitude and teleconnection strength is the late winter warming of the climatological mean SST over the tropical eastern Pacific, allowing more active and eastward extending tropical deep convection anomaly. The 2015/16 El Niño, one of the strongest events in recent history, did not bring the heavy precipitation to California anticipated based on model forecasts and experience with the previous two strong El Niños, 1982/83 and 1997/98. North American Multi-Model Ensemble (NMME) 3-month average forecasts of SST from February 1 2016, models overestimated the Niño3 SSTA, compared to what actually occurred and, consistently, forecast heavier than observed California precipitation. The too high Niño3 SSTA drove too strong deep convection anomalies in the eastern tropical Pacific, triggering a too strong teleconnection that made the forecast California precipitation too wet. Thus, the faster than forecast decay in Niño3 SST anomalies at the end of the 2015/16 El Niño is one possible reason why the event failed to bring excess precipitation to California in the late winter. Controlled GCM experiments support this hypothesis and show that the teleconnection forced by the multimodel mean forecast of 2016 February-March-April SSTAs is stronger than the one forced by the observed SSTAs. Within the NMME those models that more correctly forecast the decay of El Niño 2015/16 also more correctly forecast modest precipitation anomalies over California.