基于雪岭云杉树轮宽度重建过去339年天山中部巴音布鲁克地区夏季NDVI

doi:10.13287/j.1001-9332.202110.025

应用生态学报 ›› 2021, Vol. 32 ›› Issue (10): 3671-3679.doi: 10.13287/j.1001-9332.202110.025

基于雪岭云杉树轮宽度重建过去339年天山中部巴音布鲁克地区夏季NDVI

张权^1,2, 刘禹^1,3,4,5*, 李强^1,3,4, 孙长峰^1,3, 李腾^1,2, 李珮^1,2, 叶远达^1,2

¹中国科学院地球环境研究所黄土与第四纪地质国家重点实验室, 西安 710061;
²中国科学院大学地球与行星科学学院, 北京 100049;
³中国科学院第四纪科学与全球变化卓越创新中心, 西安 710061;
⁴中巴地球科学联合研究中心, 巴基斯坦伊斯兰堡 45320;
⁵西安交通大学人居与土木工程学院, 西安 710054

收稿日期:2021-03-31 修回日期:2021-07-24 出版日期:2021-10-15 发布日期:2022-04-15
通讯作者: * E-mail: liuyu@loess.llqg.ac.cn
作者简介:张权, 男, 1997年生, 硕士研究生。主要从事树轮生态学和树轮气候学研究。E-mail: zhangquan@ieecas.cn
基金资助:
国家自然科学基金项目(U1803245,41873021)和中国科学院战略性先导科技专项(B类)(XDB40000000)资助

Reconstruction of summer NDVI over the past 339 years based on the tree-ring width of Picea schrenkiana in Bayinbuluke, Central Tianshan, China

ZHANG Quan^1,2, LIU Yu^1,3,4,5*, LI Qiang^1,3,4, SUN Chang-feng^1,3, LI Teng^1,2, LI Pei^1,2, YE Yuan-da^1,2

¹State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China;
²College of Earth and Planetary Sciences, University of the Chinese Academy of Sciences, Beijing 100049, China;
³Center for Excellence in Quaternary Science and Global Change, Chinese Academy of Sciences, Xi'an 710061, China;
⁴China-Pakistan Joint Research Center on Earth Sciences, Islamabad 45320, Pakistan;
⁵School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, Xi'an 710054, China

Received:2021-03-31 Revised:2021-07-24 Online:2021-10-15 Published:2022-04-15
Contact: * E-mail: liuyu@loess.llqg.ac.cn
Supported by:
National Natural Science Foundation of China (U1803245, 41873021) and the Strategic Priority Research Program of Chinese Academy of Sciences (XDB40000000).

摘要/Abstract

摘要： 归一化差异植被指数(NDVI)被广泛应用于植被研究的各个领域,但由于观测时长较短,难以满足长时间尺度的研究需要。基于巴音布鲁克地区雪岭云杉建立了树轮宽度年表(STD),计算年表和NDVI同气象观测数据的相关系数。结果表明:树轮宽度指数和NDVI均与同时段的气象数据具有显著相关。结合宽度年表与6—8月NDVI间的显著正相关(r=0.7,P＜0.01,n=38),使用回归模型重建了研究区过去339年的夏季(6—8月)NDVI变化序列,在1680—2018年,重建序列有4个高植被覆盖时段(1738—1765、1786—1798、1964—1973和2000—2018年)和5个低植被覆盖时段(1690—1714、1825—1834、1850—1880、1895—1920和1945—1955年)。重建结果也反映了天山中部水文气候。与周边重建的对比显示,当开都河径流量增加,且研究区处于较为潮湿的环境时,植被覆盖相对较高,反之植被覆盖偏低。重建序列的极值也捕捉了历史文献中一系列自然灾害。混合单粒子拉格朗日综合轨迹模型(HYSPLT)后向轨迹模型和风场分析表明,NDVI异常受到西风带来的降水影响。

关键词: 天山中部, 树轮宽度, NDVI重建, 气候响应

Abstract: The normalized difference vegetation index (NDVI) is widely used in various fields of vegetation research. Due to the short observation time, however, it is difficult to meet the research needs at long time scale. Here, we established a tree-ring width chronology (STD) based on Picea schrenkiana in Bayinbuluke, and calculated the correlation coefficient of chronology and NDVI with meteorological data. The results showed that both tree-ring width index and NDVI were significantly correlated with meteorological data. Combined with the significant positive correlation between width chronology and NDVI in June-August (r=0.7, P<0.01, n=38), summer NDVI (from June to August) was reconstructed over the past 339 years using a regression model. During 1680-2018, the reconstruction series had four dense vegetation periods (1738-1765, 1786-1798, 1964-1973 and 2000-2018) and five sparse vegetation periods (1690-1714, 1825-1834, 1850-1880, 1895-1920 and 1945-1955). The reconstruction reflected the hydrological signals in the central Tianshan Mountains. The comparison with the surrounding reconstructions revealed that when the runoff of Kaidu River increased and the local environment was humid, the vegetation coverage was high; otherwise the vegetation coverage was low. The extreme value of the reconstruction series also captured a series of natural disasters recorded in historical documents. Results of HYSPLT (Hybrid Single-Particle Lagrangian Integrated Trajectory Model) backward trajectory model and wind field analysis showed that NDVI anomalies were affected by the precipitation from Westerlies.

Key words: central Tianshan, tree-ring width, NDVI reconstruction, climate response

张权, 刘禹, 李强, 孙长峰, 李腾, 李珮, 叶远达. 基于雪岭云杉树轮宽度重建过去339年天山中部巴音布鲁克地区夏季NDVI[J]. 应用生态学报, 2021, 32(10): 3671-3679.

ZHANG Quan, LIU Yu, LI Qiang, SUN Chang-feng, LI Teng, LI Pei, YE Yuan-da. Reconstruction of summer NDVI over the past 339 years based on the tree-ring width of Picea schrenkiana in Bayinbuluke, Central Tianshan, China[J]. Chinese Journal of Applied Ecology, 2021, 32(10): 3671-3679.

参考文献

[1] 朴世龙, 方精云. 1982—1999年我国陆地植被活动对气候变化响应的季节差异. 地理学报, 2003, 58(1): 119-125 [Piao S-L, Fang J-Y. Seasonal changes in vegetation activity in response to climate changes in China between 1982 and 1999. Acta Geographica Sinica, 2003, 58(1): 119-125]
[2] Chen X, Hu B, Yu R. Spatial and temporal variation of phenological growing season and climate change impacts in temperate eastern China. Global Change Biology, 2005, 11: 1118-1130
[3] 韩秀珍, 李三妹, 罗敬宁, 等. 近20年中国植被时空变化研究. 干旱区研究, 2008, 25(6): 753-759 [Han X-Z, Li S-M, Luo J-N, et al. Study on spatiotemporal change of vegetation in China since 20 years. Arid Zone Research, 2008, 25(6): 753-759]
[4] Liang E, Eckstein D, Liu H. Assessing the recent grassland greening trend in a long-term context based on tree-ring analysis: A case study in North China. Ecological Indicators, 2009, 9: 1280-1283
[5] 方欧娅, 汪洋, 邵雪梅. 基于树轮资料重建森林净初级生产力的研究进展. 地理科学进展, 2014, 33(8): 1039-1046 [Fang O-Y, Wang Y, Shao X-M. Advances in study of reconstruction of regional forest net primary productivity based on tree rings. Progress in Geographical Sciences, 2014, 33(8): 1039-1046]
[6] 张瑞波, 袁玉江, 魏文寿, 等. 天山山区树轮气候研究若干进展. 沙漠与绿洲气象, 2016, 10(4): 1-9 [Zhang R-B, Yuan Y-J, Wei W-S, et al. Research advances of dendroclimatology in Tianshan Mountains. Desert and Oasis Meteorology, 2016, 10(4): 1-9]
[7] 毛炜峄, 南庆红, 史红政. 新疆气候变化特征及气候分区方法研究. 气象, 2008, 34(10): 67-73 [Mao W-Y, Nan Q-H, Shi H-Z. Research of climatic regiona-lization with climate change in Xinjiang. Meteorological Monthly, 2008, 34: 67-73]
[8] D'arrigo RD, Malmstrom CM, Jacoby GC, et al. Correlation between maximum latewood density of annual tree rings and NDVI based estimates of forest productivity. International Journal of Remote Sensing, 2000, 21: 2329-2336
[9] Vicente-Serrano SM, Camarero JJ, Olano JM, et al. Diverse relationships between forest growth and the Normalized Difference Vegetation Index at a global scale. Remote Sensing of Environment, 2016, 187: 14-29
[10] Coulthard BL, Touchan R, Anchukaitis KJ, et al. Tree growth and vegetation activity at the ecosystem-scale in the eastern Mediterranean. Environmental Research Letters, 2017, 12: 084008
[11] Zhou Y, Yi Y, Jia W, et al. Applying dendrochronology and remote sensing to explore climate-drive in montane forests over space and time. Quaternary Science Reviews, 2020, 237: 106292
[12] Wang H, Chen F, Zhang R, et al. Seasonal dynamics of vegetation of the central Loess Plateau (China) based on tree rings and their relationship to climatic warming. Environment, Development and Sustainability, 2017, 19: 2535-2546
[13] Sun C, Liu Y, Song H, et al. Tree-ring evidence of the impacts of climate change and agricultural cultivation on vegetation coverage in the upper reaches of the Weihe River, Northwest China. Science of the Total Environment, 2020, 707: 136160
[14] 朱显亮, 李书桓, 白红英, 等. 基于太白红杉树轮宽度重建近172年太白山自然保护区7月NDVI. 应用生态学报, 2018, 29(7): 2382-2390 [Zhu X-L, Li S-H, Bai H-Y, et al. Reconstruction of July NDVI over 172 years based on tree-ring width of Larix chinensis in Taibai Mountain Nature Reserve, China. Chinese Journal of Applied Ecology, 2018, 29(7): 2382-2390]
[15] Liu R, Song Y, Liu Y, et al. Changes in the tree-ring width-derived cumulative normalized difference vegetation index over Northeast China during 1825 to 2013 CE. Forests, 2021, 12: 241
[16] 彭剑峰, 勾晓华, 陈发虎, 等. 天山东部西伯利亚落叶松树轮生长对气候要素的响应分析. 生态学报, 2006, 26(8): 2723-2731 [Peng J-F, Gou X-H, Chen F-H, et al. The responses of growth ring width variations of Larix sibirica Ledb to climatic change in eastern Tianshan Mountains. Acta Ecologica Sinica, 2006, 26(8): 2723-2731]
[17] 高琳琳, 勾晓华, 邓洋, 等. 西北干旱区树轮气候学研究进展. 海洋地质与第四纪地质, 2013, 33(4): 25-35 [Gao L-L, Gou X-H, Deng Y, et al. The advance of dendroclimatology in arid area of Northwest China. Marine Geology and Quaternary Geology, 2013, 33(4): 25-35]
[18] 刘蕊, 姜盛夏, 张同文, 等. 新疆树木年轮水文研究对比分析. 沙漠与绿洲气象, 2020, 14(3): 1-10 [Liu R, Jiang S-X, Zhang T-W, et al. Comparative analysis on dendrohydrology in Xinjiang. Desert and Oasis Meteorology, 2020, 14(3): 1-10]
[19] Zhang T, Yuan Y, Liu Y, et al. A tree-ring based precipitation reconstruction for the Baluntai region on the southern slope of the central Tianshan Mountains, China, since AD 1464. Quaternary International, 2013, 283: 55-62
[20] Zhang T, Liu Y, Zhang R, et al. Tree-ring width based streamflow reconstruction for the Kaidu River originating from the central Tianshan Mountains since AD 1700. Dendrochronologia, 2020, 61: 125700
[21] 郭艳飞, 甘淼, 杨美琳, 等. 天山东部树木径向生长与NDVI的关系. 干旱区资源与环境, 2018, 32(3): 176-180 [Guo Y-F, Gan M, Yang M-L, et al. Relationship between tree radial growth and normalized difference vegetation index in eastern Tianshan Mountains. Journal of Arid Land Resources and Environment, 2018, 32(3): 176-180]
[22] Zhang T, Zhang R, Lu B, et al. Picea schrenkiana tree-ring chronologies development and vegetation index reconstruction for the Alatau Mountains, Central Asia. Geochronometria, 2018, 45: 107-118
[23] 刘濛濛, 隆永兰. 巴音布鲁克近58 a气候变化特征分析. 干旱区地理, 2019, 42(4): 715-723 [Liu M-M, Long Y-L. Climatic variation characteristics in Bayinbuluk during the past 58 years. Arid Land Geography, 2019, 42(4): 715-723]
[24] 丁涛, 李远, 刘艳. 巴音布鲁克草原主要植被NDVI变化与气候因子的关系. 遥感信息, 2009(1): 53-59 [Ding T, Li Y, Liu Y. Relationship between the change of NDVI and the main vegetative and climate factors in Bayinbuluk Grassland. Remote Sensing Information, 2009(1): 53-59]
[25] 姚俊强, 毛炜峄, 胡文峰, 等. 1961—2015年新疆区域SPEI干旱指数数据集. 中国科学数据, 2019, 4(3): doi: 10.11922/csdata.2018.0048.zh [Yao J-Q, Mao W-Y, Hu W-F, et al. 1961-2015 Xinjiang regional SPEI drought index dataset. China Science Data, 2019, 4(3): doi: 10.11922/csdata.2018.0048.zh]
[26] Wigley TML, Briffa KR, Jones PD. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Applied Meteorology and Climatology, 1984, 23: 201-213
[27] Cook ER, Kairiukstis LA. Methods of Dendrochronology. Dordrecht: Kluwer Academic Publishers, 1990: 163-217
[28] Efron B, Stein C. The jackknife estimate of variance. Annals of Statistics, 1981, 9: 586-596
[29] Draxler RR, Hess GD. An overview of the HYSPLIT_4 modelling system for trajectories. Australian Meteorological Magazine, 1998, 47: 295-308
[30] 李明明, 李刚. 贺兰山地区植被冠层物候与树干形成层物候的关系. 应用生态学报, 2021, 32(2): 495-502 [Li M-M, Li G. Relationship between phenology of vegetation canopy and phenology of tree cambium in Helan Mountains, China. Chinese Journal of Applied Ecology, 2021, 32(2): 495-502]
[31] 刘贵峰, 臧润国, 郭仲军, 等. 不同经度天山云杉群落物种丰富度随海拔梯度变化. 应用生态学报, 2008, 19(7): 1407-1413 [Liu G-F, Zang R-G, Guo Z-J, et al. Species richness patterns of Picea schren-kiana var. tianschanica communities along an altitudinal gradient at different longitudes in Xinjiang of Northwest China. Chinese Journal of Applied Ecology, 2008, 19(7): 1407-1413]
[32] Potop V, Možný M, Soukup J. Drought evolution at various time scales in the lowland regions and their impact on vegetable crops in the Czech Republic. Agricultural and Forest Meteorology, 2012, 156: 121-133
[33] Cook ER, Anchukaitis KJ, Buckley BM, et al. Asian monsoon failure and megadrought during the last millennium. Science, 2010, 328: 486-489
[34] 李屹凯. 清代天山北麓移民垦殖与气候变化的关系. 硕士论文. 西安: 陕西师范大学, 2016 [Li Y-K. The Relationship between Immigration Reclamation and Climate Change at the Northern Foot of the Tianshan Mountains in the Qing Dynasty. Master Thesis. Xi'an: Shaanxi Normal University, 2016]
[35] 新疆社会科学院历史研究所. 新疆简史(第二册). 乌鲁木齐: 新疆人民出版社, 1980: 35 [Institute of History, Xinjiang Academy of Social Sciences. Brief History of Xinjiang (Volume 2). Urumqi: Xinjiang People's Press, 1980: 35]
[36] 路俊伟, 王乃昂, 侯迎, 等. 石羊河上游地区树轮年表与NDVI关系分析. 干旱区研究, 2012, 29(4): 667-673 [Lu J-W, Wang N-A, Hou Y, et al. Analysis on the correlation between NDVI and tree-ring width in the upper reaches of Shiyang River. Arid Zone Research, 2012, 29(4): 667-673]
[37] 王文志, 刘晓宏, 陈拓, 等. 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 [Wang W-Z, Liu X-H, Chen T, et al. Reconstruction of regional NDVI using tree-ring width chronologies in the Qilian Mountains, northwestern China. Chinese Journal of Plant Ecology, 2010, 34(9): 1033-1044]
[38] Kaufmann RK, D'arrigo RD, Paletta LF, et al. Identi-fying climatic controls on ring width: The timing of correlations between tree rings and NDVI. Earth Interactions, 2008, 12: 1-14
[39] 何吉成, 邵雪梅. 德令哈地区树轮宽度指数与草地植被指数的关系. 科学通报, 2006, 51(9): 1083-1090 [He J-C, Shao X-M. Relationship between tree ring width index and grassland vegetation index in Delingha region. Chinese Science Bulletin, 2006, 51(9): 1083-1090]
[40] 张亚宁, 张明军, 王圣杰, 等. 基于比湿订正拉格朗日模型的新疆短时强降水的水汽来源. 干旱区研究, 2019, 36(3): 698-711 [Zhang Y-N, Zhang M-J, Wang S-J, et al. Water vapor sources of short-time heavy rainfall in Xinjiang based on specific humidity-adjusted Lagrangian model. Arid Zone Research, 2019, 36(3): 698-711]
[41] 何金海, 刘芸芸, 常越. 西北地区夏季降水异常及其水汽输送和环流特征分析. 干旱气象, 2005, 23(1): 10-16 [He J-H, Liu Y-Y, Chang Y. Analysis of summer precipitation anomaly and the feature of water vapor transport and circulation in Northwest China. Arid Meteoro-logy, 2005, 23(1): 10-16]
[42] 李万莉, 王可丽, 傅慎明, 等. 区域西风指数对西北地区水汽输送及收支的指示性. 冰川冻土, 2008, 30(1): 28-34 [Li W-L, Wang K-L, Fu S-M, et al. The Interrelationship between regional westerly index and the water vapor budget in Northwest China. Journal of Glacio-logy and Geocryology, 2008, 30(1): 28-34]
[43] Yan D, Xu H, Lan J, et al. Solar activity and the wes-terlies dominate decadal hydroclimatic changes over arid Central Asia. Global and Planetary Change, 2019, 173: 53-60

基于雪岭云杉树轮宽度重建过去339年天山中部巴音布鲁克地区夏季NDVI

Reconstruction of summer NDVI over the past 339 years based on the tree-ring width of Picea schrenkiana in Bayinbuluke, Central Tianshan, China

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