DOI: 10.1016/j.gloplacha.2015.06.005
论文题名: The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon
作者: Li Q. ; Liu Y. ; Nakatsuka T. ; Song H. ; McCarroll D. ; Yang Y. ; Qi J.
刊名: Global and Planetary Change
ISSN: 0921-8181
出版年: 2015
卷: 132 起始页码: 11
结束页码: 19
语种: 英语
英文关键词: East Asian summer monsoon
; Indian summer monsoon
; Shanxi Province
; Teleconnection
; Tree-ring isotope
; Tree-ring width
Scopus关键词: Atmospheric pressure
; Atmospheric thermodynamics
; Climate change
; Climatology
; Isotopes
; Precipitation (meteorology)
; Synchronization
; East Asian summer monsoon
; Indian summer monsoon
; Shanxi Province
; Teleconnections
; Tree rings
; Tree-ring width
; Forestry
; climate variation
; coniferous tree
; decadal variation
; dendroclimatology
; El Nino-Southern Oscillation
; monsoon
; North Atlantic Oscillation
; oxygen isotope
; precipitation intensity
; proxy climate record
; reconstruction
; seasonal variation
; stable isotope
; summer
; teleconnection
; tree ring
; Isotopes
; Oxygen
; Trees
; Water Vapor
; China
; Far East
; India
; Shanxi
; Larix gmelinii var. principis-rupprechtii
; Pinus tabuliformis
英文摘要: Understanding the interactions between the East Asian summer monsoon and Indian summer monsoon is a challenging task because of the insufficient proxy records. In this study, we reconstructed a 225-year precipitation record by combining ring widths of Pinus tabulaeformis and stable oxygen isotope ratios of Larix principis-rupprechtii using a multi-proxy dendroclimatology approach in the North China. The reconstructed record explained 51.9% of the variance in the observed precipitation during 1955-2003. The precipitation series could indicate the intensity of the East Asian summer monsoon. A spatial field analysis indicated that the series was strongly correlated with the reconstructed records of the surrounding area and a large part of the Indian subcontinent. The reconstructed records were significantly and positively correlated with All Indian Precipitation records (r=. 0.32, n=. 132, p<. 0.001) and with a proxy of the Indian summer monsoon. These findings suggest that a persistent teleconnection exists between the reconstructed record and the Indian summer monsoon records from the past 225. years. The observed interannual synchronisation potentially resulted from the transport of partial water vapour from the Indian summer monsoon area to NC; however, this synchronisation could not be attributed to the El Nino-South Oscillation (ENSO). When considering an interdecadal time scale, the synchronisation with the North Atlantic Oscillation (NAO) has varied since 1779, implying that the NAO may serve as an additional atmospheric pattern that affects this teleconnection. © 2015 Elsevier B.V. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84933520623&doi=10.1016%2fj.gloplacha.2015.06.005&partnerID=40&md5=61ef39dc2cde862885d4dd1ecdf790c8
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11503
Appears in Collections: 全球变化的国际研究计划 气候变化与战略
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作者单位: State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China
Recommended Citation:
Li Q.,Liu Y.,Nakatsuka T.,et al. The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon[J]. Global and Planetary Change,2015-01-01,132.