DOI: 10.1002/joc.5730
论文题名: Intensified variability of the El Niño–Southern Oscillation enhances its modulations on tree growths in southeastern China over the past 218 years
作者: Wang L. ; Fang K. ; Chen D. ; Dong Z. ; Zhou F. ; Li Y. ; Zhang P. ; Ou T. ; Guo G. ; Cao X. ; Yu M.
刊名: International Journal of Climatology
ISSN: 8998418
出版年: 2018
卷: 38, 期: 14 起始页码: 5293
结束页码: 5304
语种: 英语
英文关键词: ENSO
; inter-annual variability
; southeast China
; tree rings
Scopus关键词: Atmospheric pressure
; Climate change
; Modulation
; O rings
; Oceanography
; Surface waters
; Asian summer monsoons
; ENSO
; Interannual variability
; Sea surface temperatures
; southeast China
; Southern oscillation
; Tree rings
; Tree-ring chronologies
; Forestry
; annual variation
; climate variation
; dendrochronology
; El Nino-Southern Oscillation
; growth response
; monsoon
; paleoclimate
; sea surface temperature
; summer
; tree ring
; China
; Fujian
; Pinus massoniana
英文摘要: 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. © 2018 Royal Meteorological Society Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/116722
Appears in Collections: 气候减缓与适应
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作者单位: Institute of Geography, Key Laboratory of Humid Subtropical Eco-geographical Process (Ministry of Education), College of Geographical Sciences, Fujian Normal University, Fuzhou, China; Regional Climate Group, Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden; International Forestry Cooperation Center, State Forestry Administration, Beijing, China; Department of Oceanography, Chonnam National University, Gwangju, South Korea; Institute of Geography and Resources of Dabie Mountains, College of Tourism Culture and Geographical Sciences, Huanggang Normal University, Huanggang, China
Recommended Citation:
Wang L.,Fang K.,Chen D.,et al. Intensified variability of the El Niño–Southern Oscillation enhances its modulations on tree growths in southeastern China over the past 218 years[J]. International Journal of Climatology,2018-01-01,38(14)