Author: ["Jinbao Li","Shang-Ping Xie","Edward R. Cook","Gang Huang","Rosanne D'Arrigo","Fei Liu","Jian Ma","Xiao-Tong Zheng"]
CITE.CC academic search helps you expand the influence of your papers.
Abstract
Our ability to predict El Niño/Southern Oscillation (ENSO) activity is hampered by the relatively short length of the instrumental record. An annually resolved record of ENSO variability over the past millennium based on tree rings indicates that ENSO amplitude varies on a 50–90 year cycle, providing an important constraint for improving predictions. The El Niño/Southern Oscillation (ENSO) is the dominant mode of interannual climate variability on Earth, alternating between anomalously warm (El Niño) and cold (La Niña) conditions in the tropical Pacific at intervals of 2–8 years1,2. The amplitude of ENSO variability affects the occurrence and predictability of climate extremes around the world3,4, but our ability to detect and predict changes in ENSO amplitude is limited by the fact that the instrumental record is too short to characterize its natural variability5,6,7,8. Here we use the North American Drought Atlas9,10—a database of drought reconstructions based on tree-ring records—to produce a continuous, annually resolved record of ENSO variability over the past 1,100 years. Our record is in broad agreement with independent, ENSO-sensitive proxy records in the Pacific and surrounding regions. Together, these records indicate that ENSO amplitude exhibits a quasi-regular cycle of 50–90 years that is closely coupled to the tropical Pacific mean state. Anomalously warm conditions in the eastern Pacific are associated with enhanced ENSO variability, consistent with model simulations11. The quasi-periodic ENSO amplitude modulation reported here offers a key observational constraint for improving models and their prediction of ENSO behaviour linked to global warming.Cite this article
Li, J., Xie, SP., Cook, E. et al. Interdecadal modulation of El Niño amplitude during the past millennium. Nature Clim Change 1, 114–118 (2011). https://doi.org/10.1038/nclimate1086 