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张齐兵


职务/职称: 研究员
联系电话: (86)-010-62836957
电子邮件: qbzhang@ibcas.ac.cn
个人网页: http://trl.ibcas.ac.cn/QBZhang.htm
课 题 组: 树木年轮与孢粉研究组

张齐兵,男,博士,研究员,博士生导师。

  19662月出生于山西省襄垣县,1988年在兰州大学生物系获学士学位,2000年在加拿大University of Victoria获博士学位。现任中国生态学会理事,中国植物学会植物生态学专业委员会委员,中国林学会森林生态专业委员会委员,中国科学探险协会理事。担任Tree-Ring ResearchDendrochronologiaAssociate Editor。迄今发表SCI刊物论文30余篇。已培养硕士和博士10名,正在指导博士生和硕士生7名。  

主要研究工作:  

  研究领域为全球变化生态学,主要运用树木年轮学方法从事以下三个方向的研究:1)森林健康历史,调查森林生态系统的自然干扰特征并揭示历史上森林衰退发生的空间范围、时间、程度及恢复特征;2)古气候重建,运用长序列(数百年乃至上千年)高分辨率(逐年甚或季节)的树木年轮资料来分析过去气候变化的特征及规律; 3)森林生长与环境因子的关系,了解环境因子之间如何相互作用并解释森林生长过程  

主持和参加的科研项目:  

从树木年轮分析极端气候下森林衰退的发生历史与恢复力,国家自然科学基金重点项目, 20141 -- 201812月),项目经费290万元,主持人 

研究论文(注*为通讯作者):  

[1] Nie, CY, Zhang, Q.-B.* and Lyu, LX. 2017. Millennium-long tree-ring chronology reveals megadroughts on the southeastern Tibetan plateau. Tree-Ring Research, 73: 1-10. 

[2] LyuLX, Zhang, Q.-B.*, Deng, X and Makinen, H. 2016. Fine-scale distribution of treeline trees and the nurse plant facilitation on the eastern Tibetan Plateau. Ecological Indicators, 66: 251-258. 

[3] Lyu, LX, Deng, X and Zhang, Q.-B.*. 2016. Elevation pattern in growth coherency on the southeastern Tibetan Plateau. PLoS ONE, 11(9) e0163201. Doi: 10.1371/journal.pone.0163201. 

[4] Zhang, C. and Zhang, Q.-B.*. 2016. Is there a link between the rise and fall of the Tuyuhun tribe (northwestern China) and climatic variations in the 4th-7th centuries AD?. Journal of Arid Environments, 125: 145-150. 

[5] Zhang, Q.-B., Evans, M.N. and Lyu, LX. 2015. Moisture dipole over the Tibetan Plateau during the past five and a half centuries. Nature Communications, 6: 8062 doi: 10.1038/ncomms9062. 

[6] Deng, X. and Zhang, Q.-B. 2015. Tree growth and climate sensitivity in open and closed forests of the southeastern Tibetan Plateau. Dendrochronologia, 33: 25-30. 

[7] Xing, P., Zhang, Q.-B. and Lv LX. 2014. Absence of late-summer warming trend over the past two and half centuries on the eastern Tibetan Plateau. Global and Planetary Change, 123: 27-35. 

[8] Duan, JP and Zhang, Q.-B. 2014. A 449 year warm season temperature reconstruction in the southeastern Tibetan Plateau and its relation to solar activity. Journal of Geophysical Research: Atmosphere, 119: 11578–11592. 

[9] Duan, JP, Zhang, Q.-B. and Lv, LX. 2013. Increased Variability in Cold-Season Temperature since the 1930s in Subtropical China. Journal of Climate, 26: 4749-4757. 

[10] Lv, LX and Zhang, Q.-B. 2013. Tree-ring based summer minimum temperature reconstruction for Yadong County at the southern edge of the Qinghai-Tibetan Plateau, China. Climate Research, 56: 91-101. 

[11] Lv, LX, Ovchinnikov, DV, Kirdyanov, AV and Zhang, Q.-B.* 2012. Comparison of temperature sensitive tree-ring chronologies in southern Tibetan Plateau and northern Siberia. Science, Technology and Development, 31(2): 152-164.  

[12] Duan, JP, Zhang, Q.-B.*, Lv, LX and Zhang, C. 2012. Regional-scale winter-spring temperature variability and chilling damage dynamics over the past two centuries in southeastern China. Climate Dynamics, 39: 919-928.   

[13] Lv, LX and Zhang, Q.-B.*. 2012. Asynchronous recruitment history of Abies spectabilis along an altitudinal gradient in the Mr.Everest region. Journal of Plant Ecology, 5 (2): 147-156.  

[14] Xing, P., Zhang, Q.-B.* and Baker, PJ. 2012. Age and radial growth pattern of four tree species in a subtropical forest of China. Trees-Structure and Function, 26: 283-290.  

[15] Shi, CM, Daux, V., Zhang, Q.-B.*, Risi, C., Hou, SG., Stievenard, M., Pierre, M., Li, ZS., and Masson-Delmotte, V. 2012. Reconstruction of southeast Tibetan plateau summer climate using tree ring 18O: moisture variability over the past two centuries. Climate of the Past, 8: 205-213.  

[16] Zhang, Q.-B.*, Li, ZS, Liu, PX and Xiao, SC. 2012. On the vulnerability of oasis forest to changing environmental conditions: perspectives from tree rings. Landscape Ecology, 27: 343-353.   

[17] Li, ZS, Zhang, Q-B*and Ma, KP. 2011. Tree-ring reconstruction of summer temperature for A.D. 1475-2003 in the central Hengduan Mountains, Northwestern Yunnan, China. Climatic Change, 110: 455-467.  

[18] Wang, X.C. and Zhang, Q.-B. 2011. Evidence of solar signals in tree rings of Smith fir from Sygera Mountain in southeast Tibet. Journal of Atmospheric and Solar-Terrestrial Physics, 73: 1959-1966.  

[19] Li, Z.S., Shi, C.M., Liu, Y.B., Zhang, J.L., Zhang, Q.-B.* and Ma, K.P. 2011. Summer mean temperature variation from 1710-2005 inferred from tree-ring data of the Baimang Snow Mountains, northwestern Yunnan, China. Climate Research, 47: 207-218.  

[20] Shi, CM, Masson-Delmotte, V., Risi, C., Eglin, T., Stievenard, M., Pierre, M., Wang, XC, Gao, J., Breon, F-M, Zhang, Q.-B.* and Daux, V. 2011. Sampling strategy and climatic implications of tree-ring stable isotopes on the southeast Tibetan Plateau. Earth and Planetary Science Letters, 301: 307-316.  

[21] Liu, YB and Zhang, Q-B.* 2010. Effect of climate on the growth of annual rings in the main roots of perennial forbs in Inner Mongolian semi-arid grassland, China. Journal of Vegetation Science, 21: 899-907.  

[22] Shi, CM, Masson-Delmotte, V., Daux, V., Li ZS and Zhang Q-B.* 2010. An unstable tree-growth response to climate in two 500 year chronologies, North Eastern Qinghai-Tibetan Plateau. Dendrochronologia, 28(4): 225-237.  

[23] Pumijumnong, N., Zhang, Q-B, Eckstein, D., Baas, P. 2009. Tree-ring research in Asia (Preface). IAWA Journal, 30: 359.  

[24] Guo, G, Li, ZS, Zhang, Q-B*, Ma, KP and Mu CL. 2009. Dendroclimatological studies of Picea Likiangensis and Tsuga Dumosa in Lijiang, China. IAWA Journal, 30: 435-441.  

[25] Wang, XC, Zhang, Q-B*, Ma, K.P. and Xiao SC. 2008. A tree-ring record of 500-year dry-wet changes in northern Tibet, China. The Holocene, 18: 579-588.  

[26] Zhang, Q-B and Shao, X.M. 2007. Tree Rings and Ecology: The 7th International Conference on Dendrochronology. Journal of Integrative Plant Biology, 49: 129-130.  

[27] Liu Y.B. and Zhang, Q-B*. 2007. Growth rings of roots in perennial forbs in Duolun grassland, Inner Mongolia, China. Journal of Integrative Plant Biology, 49: 144-149.  

[28] Zhang, Q-B* and Qiu, HY. 2007. A millennium-long tree-ring chronology of Sabina przewalskii on northeastern Qinghai-Tibetan Plateau. Dendrochronologia. 24(2-3): 91-95.  

[29] Huang, JG and Zhang, Q-B* 2007. Tree rings and climate for the last 680 years in Wulan area of northeastern Qinghai-Tibetan Plateau. Climatic Change. 80: 369-377.  

[30] Wang, T, Zhang, Q-B, and Ma, KP. 2006. Treeline dynamics in relation to climatic variability in the central Tianshan Mountains, northwestern China. Global Ecology and Biogeography 15(4): 406-415.  

[31] Zhang, Q-B*, and Hebda, RJ. 2005. Abrupt climate change and variability in the past four millennia of the southern Vancouver Island, Canada. Geophysical Research Letters, 32, L16708, doi:10.1029/2005GL022913.  

[32] He, J.S., Zhang, Q.-B., and Bazzaz, F.A. 2005. Differential drought responses between samplings and adult trees in four co-occurring species of New England. Trees-Structure and Function, 19: 442-450.  

[33] Zhang, Q.-B.*, and Hebda, R. 2004. Radial growth patterns of Douglas-fir along an elevational gradient in central coast British Columbia, Canada. Canadian Journal of Forest Research, 34:1946-1954.  

[34] Zhang, Q.-B.*, Cheng, G., Yao, T., Kang, X., and Huang, J. 2003. A 2326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan plateau. Geophysical Research Letters, 30(14), 1739, doi:10.1029/2003GL017425.  

[35] Zhang, Q.-B.*, and Alfaro, R. 2003. Spatial synchrony of the two-year cycle   budworm outbreaks in central British Columbia, Canada. Oikos, 102: 146-154.  

[36] Zhang, Q.-B., and Alfaro, R. 2002. Periodicity of two-year cycle budworm outbreaks in central British Columbia, a dendroecological analysis. Forest Science 48: 722-731.  

[37] Zhang, Q.-B., Hebda, R., Zhang, Q.-J., and Alfaro, R. 2000. Modeling tree-ring growth responses to climatic variables using artificial neural networks. Forest Science, 46: 229-239.  

[38] Zhang, Q.-B., Alfaro, R., and Hebda, R. 1999. Dendroecological studies of tree growth, climate and spruce beetle outreaks in sub-boreal forest of central British Columbia, Canada. Forest Ecology and Management, 121: 215-225.  


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