Oxygen isotope signatures preserved in tree ring cellulose as a proxy for April-September precipitation in Fujian, the subtropical region of southeast China

Chenxi Xu, Huaizhou Zheng, Takeshi Nakatsuka, Masaki Sano

Research output: Contribution to journalArticle

31 Citations (Scopus)

Abstract

A tree ring cellulose oxygen isotope (δ18O) chronology for the period 1870-2011 was established using samples from four Fokienia hodginsii trees with the aim of exploring the potential to use tree ring δ18O records to reconstruct climatic variations in Fujian, a subtropical region of southeast China. We believe that this is the first tree ring δ18O chronology from this area. Response analysis revealed that tree ring δ18O is significantly correlated with precipitation between April and September, relative humidity between August and October, and the Palmer drought severity index between April and October. Our δ18O chronology accounts for 37.4% (24.6%) of actual variation in precipitation between April and September during the period from 1951 to 2011 (1901 to 2011). Spatial correlation analysis revealed that tree ring cellulose δ18O is a suitable proxy for reconstructing April-September precipitation in Fujian, as well as in parts of Guangdong and Jiangxi, southeast China. In addition, significant correlations between δ18O chronology and the Indian summer monsoon index show that large-scale atmosphere circulation also influences tree ring δ18O. Comparisons between the tropical Pacific sea surface temperature (SST) and tree ring δ18O, during the period from 1895 to 2009, indicate that the tropical Pacific SST is positively correlated with tree ring δ18O in the study region over the last 110 years, except between 1920 and 1960. Reduced El Niño-Southern Oscillation (ENSO) variance from 1920 to 1960 may result in collapsed relationship between tree ring δ18O in Fujian and tropical Pacific SST. Key Points Tree ring oxygen isotope is a promising proxy to reconstruct rainfall ENSO influence on southeast China is low during 1920-1960 Indian summer monsoon affect tree ring oxygen isotope in southeast China

Original languageEnglish
Pages (from-to)12805-12815
Number of pages11
JournalJournal of Geophysical Research Atmospheres
Volume118
Issue number23
DOIs
Publication statusPublished - 2013 Dec 16
Externally publishedYes

Fingerprint

Oxygen Isotopes
subtropical regions
subtropical region
oxygen isotopes
tree ring
cellulose
Cellulose
oxygen isotope
China
signatures
rings
chronology
Drought
Precipitation (meteorology)
Temperature
Rain
sea surface temperature
Atmospheric humidity
Southern Oscillation
monsoons

Keywords

  • ENSO
  • Fokienia hodginsii
  • southeast China
  • tree ring cellulose d18O

ASJC Scopus subject areas

  • Atmospheric Science
  • Geophysics
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

Oxygen isotope signatures preserved in tree ring cellulose as a proxy for April-September precipitation in Fujian, the subtropical region of southeast China. / Xu, Chenxi; Zheng, Huaizhou; Nakatsuka, Takeshi; Sano, Masaki.

In: Journal of Geophysical Research Atmospheres, Vol. 118, No. 23, 16.12.2013, p. 12805-12815.

Research output: Contribution to journalArticle

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abstract = "A tree ring cellulose oxygen isotope (δ18O) chronology for the period 1870-2011 was established using samples from four Fokienia hodginsii trees with the aim of exploring the potential to use tree ring δ18O records to reconstruct climatic variations in Fujian, a subtropical region of southeast China. We believe that this is the first tree ring δ18O chronology from this area. Response analysis revealed that tree ring δ18O is significantly correlated with precipitation between April and September, relative humidity between August and October, and the Palmer drought severity index between April and October. Our δ18O chronology accounts for 37.4{\%} (24.6{\%}) of actual variation in precipitation between April and September during the period from 1951 to 2011 (1901 to 2011). Spatial correlation analysis revealed that tree ring cellulose δ18O is a suitable proxy for reconstructing April-September precipitation in Fujian, as well as in parts of Guangdong and Jiangxi, southeast China. In addition, significant correlations between δ18O chronology and the Indian summer monsoon index show that large-scale atmosphere circulation also influences tree ring δ18O. Comparisons between the tropical Pacific sea surface temperature (SST) and tree ring δ18O, during the period from 1895 to 2009, indicate that the tropical Pacific SST is positively correlated with tree ring δ18O in the study region over the last 110 years, except between 1920 and 1960. Reduced El Ni{\~n}o-Southern Oscillation (ENSO) variance from 1920 to 1960 may result in collapsed relationship between tree ring δ18O in Fujian and tropical Pacific SST. Key Points Tree ring oxygen isotope is a promising proxy to reconstruct rainfall ENSO influence on southeast China is low during 1920-1960 Indian summer monsoon affect tree ring oxygen isotope in southeast China",
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