Xuemei Shao

Chinese Academy of Sciences

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Eryuan Liang

Institute of Tibetan Plateau Research

Xiaohong Liu

Shaanxi Normal University

Haifeng Zhu

Nanjing Foreign Language School

Guofu Deng

Institute of Geographic Sciences and Natural Resources Research

Zhenju Chen

Shenyang Agricultural University

Xiaomin Zeng

Shaanxi Normal University

Guobao Xu

Northwest Institute of Eco-Environment and Resources

Lei Huang

Capital Normal University

Jinxing Lin

Beijing Forestry University

Wei Chen

Nanjing Institute of Geology and Paleontology

Cooperative Institutions

Chinese Academy of Sciences

University of Chinese Academy of Sciences

Institute of Geographic Sciences and Natural Resources Research

China Meteorological Administration

Northwest Institute of Eco-Environment and Resources

University of Arizona

University of Bern

Oeschger Centre for Climate Change Research

Lamont-Doherty Earth Observatory

Columbia University

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A 3585-YEAR RING-WIDTH DATING CHRONOLOGY OF QILIAN JUNIPER FROM THE NORTHEASTERN QINGHAI-TIBETAN PLATEAU

IAWA Journal (2009)

Xuemei Shao Shuzhi Wang Haifeng Zhu Yan Xu Eryuan Liang

This article documents the development of a precisely dated and wellreplicated long regional tree-ring width dating chronology for Qilian juniper ( Juniperus przewalskii Kom.) from the northeastern Qinghai- Tibetan Plateau. It involves specimens from 22 archeological sites, 24 living tree sites, and 5 standing snags sites in the eastern and northeastern Qaidam Basin, northwestern China. The specimens were cross-dated successfully among different groups of samples and among different sites. Based on a total of 1438 series from 713 trees, the chronology covers 3585 years and is the longest chronology by far in China. Comparisons with chronologies of the same tree species about 200 km apart suggest that this chronology can serve for dating purposes in a region larger than the study area. This study demonstrates the great potential of Qilian juniper for dendrochronological research.

Chronology

10.1163/22941932-90000226

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Citations (34)

Climatic significance of the stable carbon isotope composition of tree-ring cellulose: Comparison of Chinese hemlock (Tsuga chinensis Pritz) and alpine pine (Pinus densata Mast) in a temperate-moist region of China

Science in China Series D Earth Sciences (2007)

Xiaohong Liu Xuemei Shao Lili Wang Liangju Zhao Pu Wu

Tsuga

Dendroclimatology

Moisture stress

10.1007/s11430-007-0043-7

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August–September temperature reconstruction over the period 1792–2020 based on a tree-ring maximum latewood density

Zenodo (CERN European Organization for Nuclear Research) (2023)

Wenzheng Nie Mingqi Li Guofu Deng Xuemei Shao

We present a late summer (August–September) temperature reconstruction over the period
1792–2020 based on a tree-ring maximum latewood density (MXD) chronology for the southern Tibetan Plateau (TP).
The reconstruction explained 66.2% of the variance in the instrumental temperature records during the calibration period
1960–2020.

Tree (set theory)

10.5281/zenodo.8337358

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[Tree-ring width chronology of ancient Chinese pine in Shenyang City].

PubMed (2006)

Zhenju Chen Yu Sun Xingyuan He Xuemei Shao Wei Chen

In this paper, a master tree-ring width chronology of ancient Chinese pine in Zhaoling of Shenyang was developed, which included three chronologies, i. e., Standard, Residual, and Arstan chronology. The chronologies had significant correlations with the extreme minimum temperatures in January and April, precipitation in February, and yearly water vapor pressure. They had strong responses to the water vapor pressures in April, May, September and October, and significantly correlated with RES chronology. The chronologies had higher correlations with yearly, April, May, June, September, October and November relative humidity, among which, the correlations with yearly and May relative humidity were significant. The yearly and most monthly evaporation had negative effects on Chinese pine growth, with significant correlations between chronologies and May evaporation, but positive correlations were observed between chronologies and January evaporation. The Chinese pine growth in Shengyang was also affected by the global and hemisphere temperature anomalies. There were 32 extreme drought years corresponded to the extreme narrow or narrow rings in the chronologies during 1700 - 2004. Solar activity in 1703 - 2004 and geomagnetic activity in 1868 - 2004 also affected the chronologies, with high correlations between sunspot number and geomagnetic sudden commencement for STD chronology and ARS chronology, respectively. There were 11 yr, 23 yr and 50 yr common periodical band between solar activity and Chinese pine chronologies, and 10. 5 yr, 20 yr and 45 yr common periodical band between geomagnetic sudden commencement and Chinese pine chronologies.

Chronology

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Relationships between tree increment, climate and above-ground biomass of grass: a case study in the typical steppe, north China

Acta Oecologica (2003)

Eryuan Liang M. Vennetier Jinxing Lin Xuemei Shao

Leymus

Steppe

Aridity index

Growing season

10.1016/s1146-609x(03)00046-8

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Citations (27)

Analysis of mountain hazards in the Qilian Mountain based on tree rings

EGUGA (2017)

Yong Zhang Xuemei Shao Markus Stoffel

Tree (set theory)

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Continental-scale temperature variability during the past two millennia

Nature Geoscience (2013)

Moinuddin Ahmed Kevin J. Anchukaitis Asfawossen Asrat H. P. Borgaonkar Martina Braida

Little ice age

Centennial

Global cooling

Paleoclimatology

10.1038/ngeo1797

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Citations (1,124)

A 1437-year Precipitation History From Qilian Juniper in the Northeastern Qinghai-Tibetan Plateau

PAGES news (2005)

Xuemei Shao Eryuan Liang Lei Huang Lily Wang

Loess plateau

Qinghai lake

10.22498/pages.13.2.14

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Citations (29)

Differential response of Qilian juniper radial growth to climate variations in the middle of Qilian Mountains and the northeastern Qaidam Basin

Climatic Change (2015)

Wenzhi Wang Xiaohong Liu Xuemei Shao Dahe Qin Guobao Xu

Dendroclimatology

10.1007/s10584-015-1467-2

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Citations (10)

Changes in climatic extremes over mainland China

Climate Research (2011)

Guoyu Ren Zhaoyong Guan Xuemei Shao DY Gong

CR Climate Research Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials CR 50:105-111 (2011) - DOI: https://doi.org/10.3354/cr01067 Contribution to the CR Special: 'Changes in climatic extremes over mainland China' PREFACE Changes in climatic extremes over mainland China G. Ren1,*, Z. Guan2, X. Shao3, D. Y. Gong4 1Laboratory for Climate Studies, National Climate Centre, China Meteorological Administration, Beijing 100081, PR China 2Key Laboratory of Meteorological Disaster of the Ministry of Education, Nanjing University of Information Science and Technology, Nanjing 210044, PR China 3Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, PR China 4State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100087, PR China *Email: guoyoo@cma.gov.cn ABSTRACT: This Climate Research Special includes 10 studies reporting recent findings on change in climatic extremes in mainland China, including its characteristics, possible causes and impacts. This preface provides a summary of research results and their implications for detecting, projecting and adapting to regional climate change. KEY WORDS:Climate change · Observation · Climate model · Temperature · Precipitation · Paleo-record · Circulation anomalies · Hazard risk Full text in pdf format NextCite this article as: Ren G, Guan Z, Shao X, Gong DY (2011) Changes in climatic extremes over mainland China. Clim Res 50:105-111. https://doi.org/10.3354/cr01067 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in CR Vol. 50, No. 2-3. Online publication date: December 22, 2011 Print ISSN: 0936-577X; Online ISSN: 1616-1572 Copyright © 2011 Inter-Research.

10.3354/cr01067

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Citations (29)