NOAA/WDS Paleoclimatology - 700 Year El Niño/Southern Oscillation (ENSO) Niño3.4 Index Reconstruction

STUDY NOTES: An index of canonical El Niño/Southern Oscillation (ENSO) variability for the past seven centuries, derived from 2,222 tree-ring chronologies from Asia, New Zealand, and North and South America. The reconstruction targets the prior winter (November-January, NDJ) Niño3.4 index, and covers 1301-2005. SST anomalies (SSTAs) are relative to the mean of observed SSTs during 1971-2000.
ABSTRACT SUPPLIED BY ORIGINATOR: Predicting how the El Niño/Southern Oscillation (ENSO) will change with global warming is of enormous importance to society. ENSO exhibits considerable natural variability at interdecadal-centennial timescales. Instrumental records are too short to determine whether ENSO has changed and existing reconstructions are often developed without adequate tropical records. Here we present a seven-century-long ENSO reconstruction based on 2,222 tree-ring chronologies from both the tropics and mid-latitudes in both hemispheres. The inclusion of tropical records enables us to achieve unprecedented accuracy, as attested by high correlations with equatorial Pacific corals and coherent modulation of global teleconnections that are consistent with an independent Northern Hemisphere temperature reconstruction. Our data indicate that ENSO activity in the late twentieth century was anomalously high over the past seven centuries, suggestive of a response to continuing global warming. Climate models disagree on the ENSO response to global warming, suggesting that many models underestimate the sensitivity to radiative perturbations. Illustrating the radiative effect, our reconstruction reveals a robust ENSO response to large tropical eruptions, with anomalous cooling in the east-central tropical Pacific in the year of eruption, followed by anomalous warming one year after. Our observations provide crucial constraints for improving climate models and their future projections.