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Intensified variability of the El Niño–Southern Oscillation enhances its modulations on tree growths in southeastern China over the past 218 years
Author(s) -
Wang Lei,
Fang Keyan,
Chen Dai,
Dong Zhipeng,
Zhou Feifei,
Li Yingjun,
Zhang Peng,
Ou Tinghai,
Guo Guoyang,
Cao Xinguang,
Yu Mingtong
Publication year - 2018
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.5730
Subject(s) - climatology , dendrochronology , chronology , el niño southern oscillation , subtropics , precipitation , multivariate enso index , context (archaeology) , pinus massoniana , dendroclimatology , monsoon , southern china , east asian monsoon , environmental science , la niña , china , geography , geology , ecology , biology , meteorology , botany , archaeology
Lack of long‐term tree‐ring records in the core regions of the Asian summer monsoon in southeastern China limits our ability of evaluating the current climate change in a historical context. In this study, we developed the first 218‐year tree‐ring chronology (1798–2015) of Pinus massoniana in Zhangping area, Fujian Province, humid subtropical China. This chronology is positively correlated with winter–spring (January–March) temperature ( r = 0.359, p < .01) and summer (July–September) precipitation ( r = 0.351, p < .01). Although the correlations between our tree rings with sea surface temperatures (SSTs) are not very high, the correlation pattern is very close to the correlation pattern with the El Niño–Southern Oscillation variability (ENSO). These suggest that the ENSO could be the major large‐scale regulator on the growth of our tree rings. The strength of the correlations between our tree rings and the ENSO ( r = 0.30, N = 66) matches closely with the ENSO variability during 1950–2015. The modulations of the ENSO on regional tree growth have been the most conspicuous since the 1950s, which corresponds to its enhanced inter‐annual variability. The extreme growth anomalies match quite well with the extreme years of the moisture‐sensitive chronologies. The dry epoch from 1935 to 1958 is the most severe long‐lasting drought in our tree rings, which is a widely distributed pattern in southeastern China and is likely modulated by the La Niña‐like modes in that period.