学术研究
1. 代表性科研项目 1）国家重点基础研究发展计划(973计划)专题：冰冻圈要素的树木年轮重建及变化研究。2013年1月- 2017-12月，负责人。 2）国家自然科学基金：我国夏季风北边缘区树轮早晚材及年内δ13C和δ18O变化型季节性气候信号的识别及其气候意义。2016年1月-2019年12月，负责人。 3）国家自然科学基金：黑河流域树轮同位素记录的树木长期水分利用效率和水分来源变化。2012年1月-2015年12月，负责人。 4）中国科学院知识创新工程方向性项目(青年人才类)：横断山区树轮稳定碳氧氢同位素比率气候意义。2010年1月－2012年12月，负责人。 5）国家自然科学基金：柴达木盆地东缘祁连圆柏树轮碳氧氢同位素长序列的建立及其气候意义。2009年1月－2011年12月，负责人。 6）全球变化研究国家重大科学研究计划项目子课题：欧亚大陆典型地区树轮气候学研究。2010年1月－2014年12月，负责人。 7）国家重点基础研究发展计划（973计划）专题：西部树轮气候记录与典型冰川资料及环境要素对比。2007年8月－2011年8月，负责人。 8）国家自然科学基金：祁连山青海云杉树轮碳同位素空间变化。2005年1月－2008年12月，负责人。
2. 发表论文（*通讯作者） 1) Xiaomin Zeng, Xiaohong Liu*, Treydte K., Evans M, Wenzhi Wang, Wenling An, et al., 2017. Common variability and climate signals in intra-seasonal, earlywood, latewood and multi-decadal tree-ring δ18O from southeastern Tibet compared to δ13C: insights from observations and forward modeling. New Phytologist, doi: 10.1111/nph.14750 2) Xuanwen Zhang, Xiaohong Liu*, Qiuliang Zhang et al., 2018. Species-specific tree growth and intrinsic water-use efficiency of Dahurian larch (Larix gmelinii) and Mongolian pine (Pinus sylvestris var. mongolica) growing in a boreal permafrost region. Agricultural and Forest Meteorology, 248, 145-155 3) Xiaohong Liu *, Xuanwen Zhang, Liangju Zhao, et al., 2017. Tree-ring δ18O reveals no long-term change of atmospheric water demand since 1800 in the northern Great Higgnan Mountains, China. Journal of Geophysical Research – Atmosphere, 122，6697-6712，DOI: 10.1002/2017JD026660. 4) Dawen Li, Keyan Fang, Yingjun Li, Deliang Chen, Xiaohong Liu, et al., 2017. Climate, intrinsic water-use efficiency and tree growth over the past 150 years in humid subtropical China. PLOS one, 12(2): e0172045. 5) Ru Huang, Haifeng Zhu, Xiaohong Liu*, et al., 2017. Does increasing intrinsic water use efficiency (iWUE) stimulate tree growth at natural alpine timberline on the southeastern Tibetan Plateau? Global Planetary Change,148, 217-226 6) Bo Wang, Tuo Chen, Guobao Xu, Xiaohong Liu, et al., 2016.Alpine timberline population dynamics under climate change: a comparison between Qilian juniper and Qinghai spruce tree species in the middle Qilian Mountains of northeast Tibetan Plateau. Boreas, doi:10.1111/bor.12161 7) Liangju Zhao, Lixin Wang, Lucas A Cernusak, Xiaohong Liu, et al., 2016. Significant difference in hydrogen isotope composition between xylem and tissue water in Populus euphratica. Plant Cell & Environment, 39, 1848-1857, doi: 10.1111/pce.12753. 8) Xiaoming Zeng, Xiaohong Liu*, Evans MN, et al., 2016. Seasonal incursion of Indian Monsoon humidity and precipitation onto the southeastern Qinghai-Tibetan Plateau inferred from tree ring δ18O values with intra-seasonal resolution. Earth Planetary Science Letters, 443，9-19，doi:10.1016/j.epsl.2016.03.011. 9) Wenzhi Wang, Xiaohong Liu*, Guobao Xu, et al., 2016. Climatic instability of millennium tree-ring δ13C chronology in the northeastern part of Qaidam Basin. Global Planetary Change, 139, 165-172, 10.1016/j.gloplacha.2016.02.006 10)Guoju Wu, Xiaohong Liu*, Tuo Chen, et al. 2015. Elevation-dependent variations of tree growth and iWUE in Schrenk spruce (Picea schrenkiana) in the western Tianshan Mountains, China. Frontiers in Plant Science，6: 309. doi: 10.3389/fpls.2015.00309 11)Guobao Xu, Xiaohong Liu*, Guoju Wu, et al., 2015. Tree ring δ18O’s indication of a shift to a wetter climate since the 1880s in the western Tianshan Mountains of northwestern China. Journal of Geophysical Research - Atmosphere, 120, 6409-6425, doi: 10.1002/2014 JD023027. 12)Wenzhi Wang, Xiaohong Liu*, Xuemei Shao, et al., 2015. Differential response of the Qilian juniper radial growth to climate variations in the middle of Qilian Mountains and the northeastern Qaidam Basin. Climatic Change, 133, 237-251, doi: 10.1007/s1058 4-015-1467-2. 13)Guoju Wu, Xiaohong Liu*, Tuo Chen, et al., 2015. Long-term variation of tree growth and intrinsic water-use efficiency in Schrenk spruce with increasing CO2 concentration and climate change in China's Tianshan Mountains. Acta Physiologiae Plantarum, 37, 150, 10.1007/s11738-015-1903-y. 14)Xiaohong Liu, Wenling An, Kerstin Treydte, et al., 2015.Pooled versus separate tree-ring δD measurements, and implications for reconstruction of the Arctic Oscillation in northwestern China. Science of Total Environment, 511, 584-594, doi: 10.1016/j.scitotenv. 2015. 01. 002 15)Zhao Liangju, Wang Lixin, Liu Xiaohong et al., 2014. The patterns and implications of diurnal variations in d-excess of plant water, shallow soil water and air moisture. Hydrology and Earth System Sciences, 18, 4129-4151, doi:10.5194/hess-18-1-2014. 16)Xiaohong Liu, Wenzhi Wang, Guobao Xu, et al., 2014. Tree growth and intrinsic water-use efficiency of inland riparian forest in NW China: evaluation via δ13C and δ18O analysis of tree rings. Tree Physiology, 34(9), 966-980, doi:10.1093/treephys/tpu067. 17)Liu Xiaohong, Xu Guobao, Jussi Grießinger, et al., 2014. A shift in cloud cover over the southeastern Tibetan Plateau since 1600: evidence from regional tree-ring δ18O and its linkages to tropical oceans. Quaternary Science Reviews, 88, 55-68, doi: 10.1016/j.quascirev. 2014.01.009. 18)Zeng Xiaomin, Liu Xiaohong *, Guobao Xu, et al., 2014. Tree-ring growth recovers, but δ13C and δ15N do not change, after the removal of point-source air pollution: a case study for poplar (P. cathayana) in northwestern China. Environment Earth Sciences, 72, 2173-2182，doi: 10.1007/s12665-014-3127-7. 19)Xiaomin Zeng, Xiaohong Liu*, Guobao Xu, et al., 2014. No altitude-dependent effects on climatic signals record in tree-ring δ18O contrast to the shift in tree growth: A case study on southeastern Tibetan Plateau. Boreas, 43, 588-599, doi: 10.1111/bor.12053. 20)Wenling An, Xiaohong Liu*, Steven W. Leavitt, et al., 2014. Relative humidity history on the Batang–Litang Plateau of western China since 1755 reconstructed from tree-ring δ18O and δD data. Climatic Dynamics, 42, 2639-2654, doi: 10.1007/s00382-013-1937-z 21)Xiaohong Liu, Wenling An, Steven Leavitt, et al., 2014. Recent strengthening of correlations between tree-ring δ13C and δ18O in mesic western China: implications to climatic reconstruction and physiological responses. Global Planetary Change, 113, 23-33, doi: 10.1016/j.gloplacha.2013.12.005. 22)Guobao Xu, Xiaohong Liu*, Dahe Qin, et al., 2014. Relative humidity reconstruction for the Altay Mountains, in China using tree-ring δ18O. Chinese Science Bulletin, 59(2), 190-200, doi: 10.1007/s11434-013-0055-y 23)Guobao Xu, Xiaohong Liu*, Dahe Qin, et al. 2014. Reconstruction of a drought history for the eastern Tianshan Mountains of northwestern China since 1700 AD: evidence from tree-ring δ18O. International Journal of Climatology, 34, 3336-3347, doi: 10.1002/joc.3911. 24)Guobao Xu, Xiaohong Liu*, Dahe Qin, et al., 2014. Drought history inferred from tree-ring δ13C and δ18O at the Middle Tianshan Mountains from Northwestern China, and it’s linkage to North Atlantic Oscillation, Theory Apply Climatology, 116, 385-401, doi: 10.1007/s00704-013-0958-1. 25)Xiaohong Liu, Xiaomin Zeng, Steven Leavitt, et al., 2013. A 400-year tree-ring δ18O for the southeastern Tibetan Plateau: implications to variations of regional hydroclimate. Global Planetary Change, 104，23-33，10.1016/j.gloplacha.2013.02.005. 26)Guobao Xu, Xiaohong Liu*, Dahe Qin, et al. 2013. Climate warming and increasing atmospheric CO2 have contributed to increased intrinsic water-use efficiency on the northeastern Tibetan Plateau since 1850. Trees - Structure and Function, 27， 465-475，doi 10.1007/s00468-013-0855-3. 27)Wenzhi Wang, Xiaohong Liu*, Guobao Xu, et al., 2013. Moisture variations during last millennium reflected by tree-ring δ18O in the Qaidam Basin. Chinese Science Bulletin, 32, 3956-3961，doi: 10.1007/s11434-013-5913-0 28)Liangju Zhao, Honglang Xiao, Lixin Wang, Xiaohong Liu. 2013. The effects of short-term rainfall variability on leaf isotopic traits of desert plants in sand-binding ecosystems. Ecological Engineer 60， 116-125 29)Guoju Wu, Guobao Xu, Tuo Chen, Xiaohong Liu, et al., 2013. Age-dependent tree-ring growth responses of Schrenk spruce (Picea schrenkiana) to climate - A case study in the Tianshan Mountain, China. Dendrochronologia 31, 318-326 30)Xiaohong Liu, Wenling An, K Treydte et al., 2012. Regional Cloud Cover and SST Variations Recorded in Tree-ring δ18O of a Temperate Forest in Southwestern China. Chemical Geology, 291，104-115，doi:10.1016/j.chemgeo.2011.10.001. 31)Wenling An, Xiaohong Liu *, Steven W. Leavitt, et al., 2012. Specific climatic signals recorded in earlywood and latewood δ18O of tree rings in southwestern China. Tellus B, 64, 18703 32)Wenzhi Wang, Xiaohong Liu *, Wenling An., Guobao Xu., Xiaomin Zeng. 2012. Increased intrinsic water-use efficiency against the persisting decreased tree-radial growth in eastern part of northwestern China: causes and implications. Forest Ecology and Management, 275， 14-22，10.1016/j.foreco.2012.02.027 33)Xiaohong Liu, Liangju Zhao, Tuo Chen, et al., 2011. Combined tree-ring width and δ13C to reconstruct snowpack depth: a pilot study in the Gongga Mountain, west China. Theor Appl Climatol 103, 133-144. 34)Xiaohong Liu, Wenling An, Eryuan Liang, et al., 2011. Spatiotemporal variability in tree ring’s δ13C of Picea crassifolia in the Qilian Mountains: climatic significance and responses to rising CO2. Sciences in Cold and Arid Regions3(2), 93-102, doi: 10.3724/SP.J.1226.2011.00093 35)Xu Guobao, Chen Tuo, Liu Xiaohong*, Jin Liya, An Wenling, Wang Wenzhi. 2011. Summer temperature variations recorded in tree-ring δ13C values in the north-eastern Tibetan Plateau. Theory Apply Climatology, 105, 51-63 36)Guobao Xu, Tuo Chen, Xiaohong Liu*, Wenling An, Wenzhi Wang, Hanbo Yun. 2011. The Possible Linkages between the moisture variability on the northeastern Qaidam Basin, China Since 1800 AD and the East Asian Summer Monsoon Reflected by Tree-ring δ18O. Journal of Geophysical Research - Atmosphere 116, D09111, doi: 10.1029/2010JD015053 37)Wenzhi Wang, Xiaohong Liu*, Xuemei Shao, et al. 2011. A 200-yr temperature record from tree-ring δ13C at the Qaidam Basin of the Tibetan Plateau after identifying the optimum method to correct for changing atmospheric CO2 and δ13C. Journal of Geophysical Research 116, G04022, doi:10.1029/ 2011JG001665 38)Xiaohong Liu, Xuemei Shao, Eryuan Liang et al., 2009. Climatic significance of tree-ring δ18O in the Qilian Mountains, northwestern China and its relationship to atmospheric circulation patterns. Chemical Geology 268, 147-154 39)Xiaohong Liu, Xuemei Shao, Wang Lily, et al., 2008. Response and dendroclimatic implications of δ13C in tree rings to increasing drought on the northeastern Tibetan Plateau. Journal of Geophysical Research 113, G03015, doi: 10.1029/2007JG000610 40)Xiaohong Liu, Xuemei Shao, Liangju Zhao, et al., 2007.Dendroclimatic temperature record derived from tree-ring width and stable carbon isotope chronologies in the middle Qilian Mountains, China. Arctic Antarctic and Alpine Research39(3), 651-657 41)Xiaohong Liu, Xuemei Shao, Eryuan Liang et al., 2007. Species-dependent responses of juniper and spruce to increasing CO2 concentration and to climate in semi-arid and arid areas of northwestern China. Plant Ecology, 193: 195-209 42)Xiaohong Liu, Xuemei Shao, Lily Wang, et al., 2007. 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 50(7): 1076-1085. 43)Xiaohong Liu, Liangju Zhao, Menassie G, et al., 2007. Foliar δ13C and δ15N values of C3 plants in the Ethiopia Rift Valley and their environmental controls. Chinese Science Bulletin 52(9): 1265-1273 44)Xiaohong Liu, Dahe Qin, Xuemei Shao, et al., 2005. Temperature variations recorded in tree-rings of middle Qilian Mountains during the last millennium. Science in China, series D- Earth sciences 2005, 8: 521-529 45)Xiaohong Liu, Dahe Qin, Xuemei Shao, et al., 2003. Climatic significance of stable carbon isotope in tree-rings of Abies spectabibis in south-eastern Tibet. Chinese Science Bulletin 48(18): 2000-2004 46)Eryuan Liang, Xuemei Shao, Xiaohong Liu. 2009. Annual precipitation variation inferred from tree rings since AD 1770 for the western Qilian Mountains, northern Tibetan Plateau. Tree-ring Research 65(2)：95-103 47)Eryuan Liang, Xiaohong Liu, Yujiang Yuan, et al. 2006. The 1920s drought recorded by tree rings and historical documents in the semi-arid and arid areas of northern China. Climatic Change 70: 403-432 48)Eryuan Liang, Xuemei Shao, D Eckstein, Xiaohong Liu. 2006. Topography- and species-dependent growth responses of Sabina przewalskii and Picea crassifolia to climate on the northeast Tibetan Plateau. Forest Ecology and management 26: 268-277 49)Eryuan Liang, Xuemei Shao, D Eckstein, Xiaohong Liu. 2010. Spatial variability of tree growth along a latitudinal transect in the Qilian Mountains, northeastern Tibetan Plateau. Can J For Research 40: 200-211 50)Liangju Zhao, Honglang Xiao, Xiaohong Liu, et al., 2010. Correlations between δ13C and δ15N in C4 and C3 plants of natural and artificial sandbinding microhabitats in the Tengger Desert of China. Ecological Informatics 5, 177-186 51)Liangju Zhao, Honglang Xiao, Xiaohong Liu, et al. 2007. Correlations of foliar Delta with K concentration and ash content in sand-fixing plants in the Tengger Desert of China: patterns and implications. Environmental Geology 51(6): 1049-1056 52)Liangju Zhao, Honglang Xiao, Xiaohong Liu. 2007. Relationships between carbon isotope discrimination and yield of spring wheat under different water and nitrogen levels. Journal of Plant Nutrition, 30(6), 947-963. 53)Liangju Zhao, Honglang Xiao, Xiaohong Liu, et al., 2007. Foliar stable carbon isotope discrimination and nutrients contents in two desert plant species. Polish Journal of Ecology, 55(1), 57-66 54)Liangju Zhao, Honglang Xiao, Xiaohong Liu. 2006. Variations of foliar carbon isotope discrimination and nutrient concentrations in Artemisia ordosica and Caragana korshinskiiat at the southeastern margin of China’s Tengger Desert. Environ Geol., 50, 285-294 55)张轩文，杨丽，刘晓宏*，等（2017）大兴安岭北部多年冻土区落叶松和樟子松生长的气候响应差异研究。冰川冻土，39（1）, 165-173 56)刘晓宏, 徐国保, 王文志, 等 (2015) 树轮稳定同位素记录：进展、问题及展望。第四纪研究，35(5), 1245-1260 57)徐国保，刘晓宏*，陈拓，等(2015) 中国西部树木年轮δ１８Ｏ的气候信号。第四纪研究，35(5), 1218-1216 58)王文志，刘晓宏*，徐国保, 等（2013）柴达木盆地树轮δ18O记录的过去1000年湿度变化。科学通报，58, 3458-3463. 59)徐国保，刘晓宏*，秦大河，等(2014) 树木年轮δ18O记录的中国西北阿尔泰山区相对湿度变化。科学通报，59，1478. 60)刘晓宏, 刘禹, 徐国保, 等 (2010) 树木年轮稳定同位素分析样品前处理方法探讨. 冰川冻土, 32(6): 1242-1250. 61)刘晓宏, 安文玲, 梁尔源, 等 (2010) 祁连山青海云杉树轮δ13C的时空变化及其气候意义. 冰川冻土, 32(04): 666-676. 62)王文志, 刘晓宏*, 陈拓, 等 (2010). 基于祁连山树轮宽度指数的区域NDVI重建. 植物生态学报, 2010，34(9): 1033-1044. 63)徐国保, 刘晓宏*, 陈拓, 等（2009）新疆哈密八大石森林上限树轮记录的温度变化信息. 山地学报，04: 402-410. 64)安文玲, 刘晓宏*, 陈拓,等（2009）云南丽江树轮δ18O记录的大气环流变化信息。地理学报64(09): 1103-1112. 65)贠汉伯, 陈拓, 刘晓宏, 等 (2010) 祁连山青海云杉叶片δ13C特征及其与生理指标关系. 冰川冻土, 32(1): 152-156. 66)刘晓宏, 邵雪梅, 王丽丽, 等 (2007) 温暖湿润区铁杉和高山松树轮δ13C的气候意义. 中国科学 D 辑: 地球科学, 37(4): 544-552. 67)刘晓宏，赵良菊，Menassie Gasaw，等 (2007) 东非大裂谷埃塞俄比亚段内C3植物叶片的δ13C和δ15N及其环境指示意义。科学通报，52(2): 199-206 68)刘晓宏，秦大河，邵雪梅，等 (2004) 祁连山中部近千年温度变化的树轮记录。中国科学（D）: 地球科学，34(1)：89－95 69)刘晓宏，秦大河，邵雪梅，等 (2003) 西藏喜马拉雅冷杉年轮δ13C气候意义。科学通报, 48(11): 1209-1213 70)刘晓宏，秦大河，邵雪梅，等 (2002) 西藏林芝冷杉树轮稳定碳同位素对气候的响应。冰川冻土，24（5）：574－57 71)刘晓宏，秦大河，邵雪梅，等。(2003) 西藏林芝地区自公元1650年来降水变化及突变分析。冰川冻土, 25(4): 448-452
3. 人才培养及科研奖励 指导研究生7名：现在读硕士生2人，博士生1人, 合作博士后2人。指导研究生获中国科学院优秀博士论文1人次，中国科学院院长特别奖1人次，院长优秀奖3人次，获研究生国家奖学金3人次，获卢嘉锡优秀研究生奖1人次，获朱李月华优秀博士生奖2人次，获BHBP优秀研究生奖1人次。获2014年中科院兰州分院优秀研究生导师和2014年中科院BHPB导师科研奖。
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