[1] 高佳妮. 苏峪口国家森林公园树木径向生长监测及模拟研究. 硕士论文. 北京: 中国科学院大学, 2019[Gao J-N. Monitoring and Simulation of Tree Radial Growth in Suyukou National Forest Park. Master Thesis. Beijing: University of Chinese Academy of Sciences, 2019] [2] Yang B, Wang JL, Liu JJ. A 1556 year-long early summer moisture reconstruction for the Hexi Corridor, Northwestern China. Science China Earth Science, 2019, 62: 953-963 [3] 马柱国, 符淙斌, 杨庆, 等. 关于我国北方干旱化及其转折性发生. 大气科学, 2018, 42(4): 951-961 [Ma Z-G, Fu C-B, Yang Q, et al. Drying trend in northern China and its shift during 1951-2016. Chinese Journal of Atmospheric Sciences, 2018, 42: 951-961] [4] Wang XF, Yang B, Li G. Drought-induced tree growth decline in the desert margins of Northwestern China. Dendrochronologia, 2020, 60: 125685 [5] Zeng XM, Wei CF, Liu XH, et al. Qinghai spruce (Picea crassifolia) and Chinese pine (Pinus tabuliformis) show high vulnerability and similar resilience to early-growing-season drought in the Helan Mountains, China. Ecological Indicators, 2020, 110: 105871 [6] IPCC. Climate Change 2014: Mitigation of Climate Change: Working Group Ⅲ Contribution to the IPCC Fifth Assessment Report. Cambridge, UK: Cambridge University Press, 2014 [7] Chen L, Huang JG, Ma QQ, et al. Spring phenology at different altitudes is becoming more uniform under global warming in Europe. Global Change Biology, 2018, 24: 3969-3975 [8] Wang XF, Yang B. Divergent tree radial growth at alpine coniferous forest ecotone and corresponding response to climate change in northwestern China. Ecological Indicators, 2021, 121: 107052 [9] Zhang LN, Jiang Y, Zhao SD, et al. Different responses of the radial growth of conifer species to increasing temperature along altitude gradient: Pinus tabuliformis in the Helan Mountains (Northwestern China). Polish Journal of Ecology, 2016, 64: 509-525 [10] 江源, 杨艳刚, 董满宇, 等. 芦芽山林线白杄与华北落叶松径向生长特征比较. 应用生态学报, 2009, 20(6): 1271-1277 [Jiang Y, Yang Y-G, Dong M-Y, et al. Stem radius growth of Picea meyeri and Larix principis-rupprechtii nearby the tree-line of Luya Mountain. Chinese Journal of Applied Ecology, 2009, 20: 1271-1277] [11] 王章勇, 杨保, 秦春, 等. 树木径向生长机制监测和模拟研究进展. 中国沙漠, 2011, 31(3): 780-787 [Wang Z-Y, Yang B, Qin C, et al. Research progress of the monitor and model of stem radius growth mechanism. Journal of Desert Research, 2011, 31(3): 780-787] [12] Wang ZY, Yang B, Deslauriers A, et al. Intra-annual stem radial increment response of Qilian juniper to temperature and precipitation along an altitudinal gradient in northwestern China. Trees-Structure and Function, 2015, 29: 25-34 [13] Jiang Y, Wang BQ, Dong MY, et al. Response of daily stem radial growth of Platycladus orientalis to environmental factors in a semi-arid area of North China. Trees-Structure and Function, 2015, 29: 87-96 [14] Zhang RB, Yuan YJ, Gou XH, et al. Intra-annual radial growth of Schrenk spruce (Picea schrenkiana Fisch. et Mey) and its response to climate on the northern slopes of the Tianshan Mountains. Dendrochronologia, 2016, 40: 36-42 [15] Gao JN, Yang B, He MH, et al. Intra-annual stem radial increment patterns of Chinese pine, Helan Mountains, Northern Central China. Trees-Structure and Function, 2019, 33: 751-763 [16] 王小明, 刘振生, 李志刚, 等. 宁夏贺兰山国家级自然保护区综合科学考察. 银川: 阳光出版社, 2011 [Wang X-M, Liu Z-S, Li Z-G, eds. Comprehensive Scientific Investigation of Helanshan National Nature Reserve in Ningxia. Yinchuan: Sunshine Press, 2011] [17] Deslauriers A, Morin H, Urbinati C, et al. Daily wea-ther response of balsam fir (Abies balsamea (L.) Mill.) stem radius increment from dendrometer analysis in the boreal forests of Quebec (Canada). Trees-Structure and Function, 2003, 17: 477-484 [18] Bogeat-Triboulot MB, Mikael B, Jenny R, et al. Gra-dual soil water depletion results in reversible changes of gene expression, protein profiles, ecophysiology, and growth performance in Populus euphratica, a poplar growing in arid regions. Plant Physiology, 2007, 143: 876-892 [19] Claeys H, Inzé D. The agony of choice: How plants balance growth and survival under water-limiting conditions. Plant Physiology, 2013, 162: 1768-1779 [20] Zhang QB, Cheng GD, Yao TD, et al. A 2326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophysical Research Letters, 2003, 30: 1739 [21] 秦宁生, 邵雪梅, 靳立亚, 等. 青海南部高原圆柏年轮指示的近500年来气候变化. 科学通报, 2013, 48(19): 2068-2072 [Qin N-S, Shao X-M, Jin L-Y, et al. Climate change over southern Qinghai Plateau in the past 500 years recorded in Sabina tibetica tree rings. Chinese Science Bulletin, 2003, 48(19): 2068-2072] [22] Li JB, Cook ER, D' Arrigo R, et al. Common tree growth anomalies over the northeastern Tibetan Plateau during the last six centuries: Implications for regional moisture change. Global Change Biology, 2008, 14: 2096-2107 [23] Gou XH, Deng Y, Gao LL, et al. Millennium tree-ring reconstruction of drought variability in the eastern Qilian Mountains, northwest China. Climate Dynamic, 2015, 45: 1761-1770 [24] Li JB, Chen FH, Cook ER, et al. Drought reconstruction for north central China from tree rings: The value of the Palmer drought severity index. International Journal of Climatology, 2007, 27: 903-909 [25] 蔡秋芳. 贺兰山油松生长对三种不同水分指数的响应及1—7月Walter指数重建. 海洋地质与第四季地质, 2009, 29(6): 131-136 [Cai Q-F. Response of Pinus tabuliformis tree-ring growth to three moisture indices and January to July Walter index reconstruction in Helan Mountain. Marine Ecology & Quaternary Geology, 2009, 29(6): 131-136] [26] Yang B, Qin C, Wang JL, et al. A 3500-year tree-ring record of annual precipitation on the northeastern Tibe-tan Plateau. Proceeding of the National Academy of Science of the United States of America, 2014, 111: 2903-2908 [27] Peng CH, Ma ZH, Lei XD, et al. A drought-induced pervasive increase in tree mortality across Canada boreal forest. Nature Climate Change, 2011, 1: 467-471 [28] Allen CD, Macaady AK, Chenchouni H, et al. A global overview drought and heat-induced tree mortality reveals emerging climate change risks for forests. Forest Ecology and Management, 2010, 259: 660-884 |