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posted on 2020-06-09, 17:28 authored by Dai Chen, Feifei Zhou, Zhipeng Dong, A’ying Zeng, Tinghai Ou, Keyan Fang

a) Correlations calculated between the tree-ring δ18O chronology and climate variables recorded by Shanghang meteorological station from previous November to current October during the period of 1960–2014. M-A symbolizes the combined months from May to August. Stars indicate the 95% confidence level; b) Relationship between the δ18O chronology and the observed EASM index for the period of 1948–2014.

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    Pinus massoniana treesmiddle Yangtze River basincore EASM areasEl Ni ño OscillationENSO variability coheresanthropogenic impactENSO variabilitytree-ring cellulose δ 18 O recordsEASM reconstructionmonsoon intensity200- yearaerosol emissionsdecadal variationsEASM-ENSO connectionstree-ring δ 18 Oδ 18 O chronology accountscore regionssummer monsoonEASM-ENSO relationshipEast Asia summer monsoon

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