globalchange  > 气候变化与战略
DOI: 10.1016/j.earscirev.2019.02.012
论文题名:
Recent advances in dendroclimatology in China
作者: He M.; Yang B.; Bräuning A.; Rossi S.; Ljungqvist F.C.; Shishov V.; Grießinger J.; Wang J.; Liu J.; Qin C.
刊名: Earth Science Reviews
ISSN: 00128252
出版年: 2019
卷: 194
起始页码: 521
结束页码: 535
语种: 英语
中文关键词: China ; Climate change ; Dendroclimatology ; Hydroclimate reconstructions ; Temperature reconstructions ; Tree growth
英文关键词: air temperature ; climate change ; coniferous tree ; dendroclimatology ; paleoclimate ; reconstruction ; spatial analysis ; China ; Qinghai-Xizang Plateau ; Coniferales
英文摘要: Considerable progress has been made in dendroclimatological research in China during the period 2000–2017, including a significant increase in the spatial coverage of tree-ring chronologies developed for paleoclimatic research. New tree-ring sampling sites have been established across the Tibetan Plateau, as well as the northeastern and sub-tropical eastern parts of China. Most of the studies use coniferous trees, although different plant functional types (e.g., broadleaf species and shrubs) have also been increasingly investigated. Tree-ring chronologies longer than 600 years, however, are mostly found on the Tibetan Plateau, with the longest one extending back to 2637 BCE (before Common Era). Most tree-ring records in the eastern parts of China are <400 years long. Tree-ring width is the most commonly studied parameter, although stable isotope ratios and wood density data have also been obtained for specific sites. Stable oxygen isotope data frequently shares a common hydroclimate signal, whereas the climate or environmental signals remain inconsistent for the few available stable carbon isotope records. In general, tree-ring width-based temperature reconstructions originate from higher elevation sites (i.e., treeline) compared to hydroclimate reconstructions. Precipitation or drought reconstructions are mainly obtained from regions with an annual precipitation of <800 mm. Most of the tree-ring reconstructions are based on individual site or local-scale chronologies, although a limited number of regional-scale and field reconstructions have been produced. The most prominent identified characteristics of the recent advances in dendroclimatological research for China have manifested in aspects such as an expanded network of sampling sites, improved climate reconstruction methodology, and improved uncertainty estimations in the latter. Furthermore, the traditional statistical-based tree growth–climate relationships have been supplemented by monitoring and modeling approaches. Based on the progress from 2000 to 2017, and on the research potential of the country in this field, we expect additional widening of the dendroclimatological investigations in China during the coming years. © 2019
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165824
Appears in Collections:气候变化与战略

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作者单位: Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China; Institute of Geography, Friedrich-Alexander-University of Erlangen-Nürnberg, Erlangen, 91058, Germany; Département des Sciences Fondamentales, Université du Québec à Chicoutimi, Chicoutimi, G7H 2B1, Canada; Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, 51065, China; Department of History, Stockholm University, Stockholm, 106 91, Sweden; Bolin Centre for Climate Research, Stockholm University, Stockholm, 106 91, Sweden; Department of Geography, University of Cambridge, Cambridge, CB2 3EN, United Kingdom; Mathematical Methods and Information Technology Department, Siberian Federal University, Krasnoyarsk, 660075, Russian Federation

Recommended Citation:
He M.,Yang B.,Bräuning A.,et al. Recent advances in dendroclimatology in China[J]. Earth Science Reviews,2019-01-01,194
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