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中国西部树木年轮δ18O的气候信号

DOI: 10.11928/j.issn.1001-7410.2015.05.18, PP. 1218-1226

Keywords: 树木年轮,稳定氧同位素,气候信号,空间变化,中国西部

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Abstract:

树轮稳定氧同位素比率(δ18O)记录在区域气候重建方面具有一定优势。树轮δ18O记录受树木生长趋势的影响较小,保留了丰富的低频信号,对区域气候变化有较一致的响应。通过对比我国西部1901~2004年树轮δ18O平均值和降水δ18O空间分布特征发现,两者空间分布存在一定的相似性。在青藏高原南部树轮δ18O为低值,而青藏高原北部树轮δ18O为高值。树轮δ18O平均值随树轮样点纬度的向北偏移而增大。树轮δ18O与相邻气象站记录响应分析表明,树轮δ18O和生长季的温度呈显著正相关,与生长季降水和相对湿度呈现显著负相关关系。旋转经验正交函数分析和空间响应分析表明,树轮δ18O在我国西风影响区的新疆北部主要反映与区域干湿变化相关的气候信号;树轮δ18O在西南季风影响的藏东南区主要反映区域水文气候变化信息;然而,在季风和西风影响的交汇区域,树轮δ18O的区域气候信号相对较弱。

References

[1]  2 刘 禹, 蔡秋芳, 宋慧明. 关于青藏高原2485年温度的季节和空间代表性问题. 第四纪研究, 2013, 33 (1):108~114 Liu Yu, Cai Qiufang, Song Huiming. Seasonal and spatial representativeness of the tree-ring based 2485-year annual mean temperature reconstruction in the northeastern Tibetan Plateau. Quaternary Sciences, 2013, 33 (1):108~114
[2]  3 勾晓华, 杨梅学, 彭剑峰等. 树轮记录的阿尼玛卿山区过去830年夏半年最高温变化. 第四纪研究, 2006, 26 (6):991~998 Gou Xiaohua, Yang Meixue, Peng Jianfeng et al. Maximum temperature reconstruction for Animaqing Mountains over past 830 years based on tree-ring records. Quaternary Sciences, 2006, 26 (6):991~998
[3]  4 杨 保. 树轮记录的小冰期以来青藏高原气候变化的时空特征. 第四纪研究, 2012, 32 (1):81~94 Yang Bao. Spatial and temporal patterns of climate variations over the Tibetan Plateau during the period 1300~2010. Quaternary Sciences, 2012, 32 (1):81~94
[4]  5 袁玉江, 魏文寿, 陈 峰等. 天山北坡乌鲁木齐河年径流总量的树轮重建. 第四纪研究, 2013, 33 (3):501~510 Yuan Yujiang, Wei Wenshou, Chen Feng et al. Tree-ring reconstruction of annual total runoff for the ürümqi River on the northern slope of Tien Shan Mountains. Quaternary Sciences, 2013, 33 (3):501~510
[5]  6 蔡秋芳, 刘 禹. 山西五鹿山油松树轮宽度年表的建立及过去百余年5~6月平均气温变化. 第四纪研究, 2013, 33 (3):511~517 Cai Qiufang, Liu Yu. The development of a tree-ring width chronology and the May~June mean temperature variability in Wulu Mountain, north-Central China. Quaternary Sciences, 2013, 33 (3):511~517
[6]  7 李宗善, 刘国华, 傅伯杰等. 利用树木年轮宽度资料重建川西米亚罗地区过去200年夏季温度的变化. 第四纪研究, 2011, 31 (3):522~534 Li Zongshan, Liu Guohua, Fu Bojie et al. Tree ring-based summer temperature reconstruction over the past 200 years in Miyaluo of western Sichuan, China. Quaternary Sciences, 2011, 31 (3):522~534
[7]  8 Liu Xiaohong, Xu Guobao, Grieinger J et al. 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, 2014, 88 :55~68
[8]  9 Roden J S, Lin G, Ehleringer J R. A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose. Geochimica et Cosmochimica Acta, 2000, 64 (1):21~35
[9]  10 Sternberg L, Deniro M J D. Biogeochemical implications of the isotopic equilibrium fractionation factor between the oxygen atoms of acetone and water. Geochimica et Cosmochimica Acta, 1983, 47 (12):2271~2274
[10]  11 Sternberg L, Anderson W T, Morrison K. Separating soil and leaf water 18 O isotopic signals in plant stem cellulose. Geochimica et Cosmochimica Acta, 2003, 67 (14):2561~2566
[11]  12 Sternberg L. Oxygen stable isotope ratios of tree-ring cellulose:The next phase of understanding. New Phytologist, 2009, 181 (3):553~562
[12]  13 Waterhouse J S, Switsur V R, Barker A C et al. Oxygen and hydrogen isotope ratios in tree rings:How well do models predict observed values?Earth and Planetary Science Letters, 2002, 201 (2):421~430
[13]  14 Deniro M J, Epstein S. Isotopic composition of cellulose from aquatic organisms. Geochimica et Cosmochimica Acta, 1981, 45 (10):1885~1894
[14]  15 Porter T J, Pisaric M F, Field R D et al. Spring-summer temperatures since AD 1780 reconstructed from stable oxygen isotope ratios in white spruce tree-rings from the Mackenzie Delta, Northwestern Canada. Climate Dynamics, 2014, 42 (3~4):771~785
[15]  16 Libby L M, Pandolfi L J, Payton P H et al. Isotopic tree thermometers. Nature, 1976, 261 :284~288
[16]  29 Shi Chunming, Daux V, Zhang Qibing et al. Reconstruction of southeast Tibetan Plateau summer climate using tree ring δ18O:Moisture variability over the past two centuries. Climate of the Past, 2012, 8 :205~213
[17]  30 Liu Xiaohong, Zeng Xiaomin, Leavitt S W et al. A 400-year tree-ring δ18O chronology for the southeastern Tibetan Plateau:Implications for inferring variations of the regional hydroclimate. Global and Planetary Change, 2013, 104 :23~33
[18]  38 Vicente-Serrano S M, Gouveia C, Camarero J J et al. Response of vegetation to drought time-scales across global land biomes. Proceedings of the National Academy of Sciences of the United States of America, 2013, 110 (1):52~57
[19]  39 Vicente-Serrano S M, Beguería S, López-Moreno J I et al. A new global 0.5° gridded dataset(1901~2006)of a multiscalar drought index:Comparison with current drought index datasets based on the Palmer drought severity index. Journal of Hydrometeorology, 2010, 11 (4):1033~1043
[20]  49 Feng Xiahong, Reddington A L, Faiia A M et al. The changes in north American atmospheric circulation patterns indicated by wood cellulose. Geology, 2007, 35 (2):163~166
[21]  50 安文玲, 刘晓宏, 陈 拓等. 云南丽江树轮 δ18O记录的大气环流变化信息. 地理学报, 2009, 64 (9):1103~1112 An Wenling, Liu Xiaohong, Chen Tuo et al. Atmospheric circulation information recorded in tree-ring δ18O at Lijiang, Yunnan Province. Acta Geographica Sinica, 2009, 64 (9):1103~1112
[22]  51 Liu Xiaohong, An Wenling, Leavitt S W et al. Recent strengthening of correlations between tree-ring δ 13 C and δ18O in mesic Western China:Implications to climatic reconstruction and physiological responses. Global and Planetary Change, 2014, 113 :23~33
[23]  53 Liu Jianrong, Song Xianfang, Sun Xiaomin et al. Isotopic composition of precipitation over arid Northwestern China and its implications for the water vapor origin. Journal of Geographical Sciences, 2009, 19 (2):164~174
[24]  1 邵雪梅, 王树芝, 徐 岩等. 柴达木盆地东北部3500年树轮定年年表的初步建立. 第四纪研究2007, 27 (4):477~485 Shao Xuemei, Wang Shuzhi, Xu Yan et al. A 3500-year master tree-ring dating chronology from the northeastern part of the Qaidam Basin. Quaternary Sciences, 2007, 27 (4):477~485
[25]  17 Sidorova O V, Siegwolf R T W, Myglan V S et al. The application of tree-rings and stable isotopes for reconstructions of climate conditions in the Russian Altai. Climatic Change, 2013, 120 (1~2):153~167
[26]  18 Rinne K T, Loader N J, Switsur V R et al.400-year May-August precipitation reconstruction for Southern England using oxygen isotopes in tree rings. Quaternary Science Reviews, 2013, 60 :13~25
[27]  19 Treydte K S, Schleser G H, Helle G et al. The twentieth century was the wettest period in Northern Pakistan over the past millennium. Nature, 2006, 440 :1179~1182
[28]  20 Xu Guobao, Liu Xiaohong, Qin Dahe et al. Tree-ring δ18O evidence for the drought history of eastern Tianshan Mountains, Northwest China since 1700 AD. International Journal of Climatology, 2014, 34 (12):3336~3347
[29]  21 An Wenling, Liu Xiaohong, Leavitt S W et al. Relative humidity history on the Batang-Litang Plateau of Western China since 1755 reconstructed from tree-ring δ18O and δD. Climate Dynamics, 2014, 42 (9~10):2639~2654
[30]  22 Liu Xiaohong, Shao Xuemei, Liang Eryuan et al. Climatic significance of tree-ring δ18O in the Qilian Mountains, Northwestern China and its relationship to atmospheric circulation patterns. Chemical Geology, 2009, 268 (1~2):147~154
[31]  23 Liu Yu, Cai Qiufang, Liu Weiguo et al. Monsoon precipitation variation recorded by tree-ring δ18O in arid Northwest China since AD 1878. Chemical Geology, 2008, 252 (1~2):56~61
[32]  24 Treydte K, Frank D, Esper J et al. Signal strength and climate calibration of a European tree-ring isotope network. Geophysical Research Letters, 2007, 34 (24):L24302
[33]  25 Saurer M, Schweingruber F, Vaganov E A et al. Spatial and temporal oxygen isotope trends at the northern tree-line in Eurasia. Geophysical Research Letters, 2002, 29 (9):GL013739
[34]  26 Sano M, Xu C, Nakatsuka T. A 300-year Vietnam hydroclimate and ENSO variability record reconstructed from tree ring δ18O. Journal of Geophysical Research, 2012, 117 (D12):D12115
[35]  27 Grieinger J, Br?uning A, Helle G et al. Late Holocene Asian summer monsoon variability reflected by δ18O in tree-rings from Tibetan junipers. Geophysical Research Letters, 2011, 38 (3):L03701
[36]  28 Xu Hai, Hong Yetang, Hong Bin. Decreasing Asian summer monsoon intensity after 1860 AD in the global warming epoch. Climate Dynamics, 2012, 39 (7~8):2079~2088
[37]  31 Xu Guobao, Chen Tuo, Liu Xiaohong et al. Potential linkages between the moisture variability in the northeastern Qaidam Basin, China, since 1800 and the East Asian summer monsoon, as reflected by tree-ring δ18O. Journal of Geophysical Research, 2011, 116 (D9):D09111
[38]  32 Qin Chun, Yang Bao, Br?uning A et al. Drought signals in tree-ring stable oxygen isotope series of Qilian Juniper from the arid northeastern Tibetan Plateau. Global and Planetary Change, 2015, 125 :48~59
[39]  33 Wang Wenzhi, Liu Xiaohong, Xu Guobao et al. Moisture variations over the past millennium characterized by Qaidam Basin tree-ring δ18O. Chinese Science Bulletin, 2013, 58 (32):3956~3961
[40]  34 Xu Guobao, Liu Xiaohong, Qin Dahe et al. Drought history inferred from tree ring δ 13 C and δ18O in the central Tianshan Mountains of China and linkage with the North Atlantic Oscillation. Theoretical and Applied Climatology, 2014, 116 (3~4):385~401
[41]  35 Xu Guobao, Liu Xiaohong, Qin Dahe et al. Relative humidity reconstruction for Northwestern China''s Altay Mountains using tree-ring δ18O. Chinese Science Bulletin, 2014, 59 (2):190~200
[42]  36 Liu Xiahong, An Wenling, Treydte K et al. Tree-ring δ18O in Southwestern China linked to variations in regional cloud cover and tropical sea surface temperature. Chemical Geology, 2012, 291 :104~115
[43]  37 刘晓宏, 刘 禹, 徐国保等. 树木年轮稳定同位素分析样品前处理方法探讨. 冰川冻土, 2010, 32 (6):1242~1250 Liu Xiaohong, Liu Yu, Xu Guobao et al. Pretreatment of the tree-ring samples for stable isotope analysis. Journal of Glaciology and Geocryology, 2010, 32 (6):1242~1250
[44]  40 Vicente-Serrano S M, Beguería S, López-Moreno J I. A multiscalar drought index sensitive to global warming: The standardized precipitation evapotranspiration index. Journal of Climate, 2010, 23 (7):1696~1718
[45]  41 Vicente-Serrano S M, Beguería S, Lorenzo-Lacruz J et al. Performance of drought indices for ecological, agricultural, and hydrological applications. Earth Interactions, 2012, 16 (10):1~27
[46]  42 Tao Hui, Borth H, Fraedrich K et al. Drought and wetness variability in the Tarim River basin and connection to large-scale atmospheric circulation. International Journal of Climatology, 2014, 34 (8):2678~2684
[47]  43 Vicente-Serrano S M, López-Moreno J I, Drummond A et al. Effects of warming processes on droughts and water resources in the NW Iberian Peninsula(1930~2006). Climate Research, 2011, 48 (2~3):203~212
[48]  44 Li Qiang, Nakatsuka T, Kawamura K et al. Regional hydroclimate and precipitation δ18O revealed in tree-ring cellulose δ18O from different tree species in semi-arid Northern China. Chemical Geology, 2011, 282 (1):19~28
[49]  45 Leonelli G, Pelfini M, Battipaglia G et al. First detection of glacial meltwater signature in tree-ring δ18O:Reconstructing past major glacier runoff events at Lago Verde(Miage Glacier, Italy). Boreas, 2014, 43 (3):600~607
[50]  46 Managave S R, Ramesh R. Isotope dendroclimatology:A review with a special emphasis on tropics. In:Baskaran M ed. Handbook of Environmental Isotope Geochemistry, Advances in Isotope Geochemistry. Berlin Heidelberg:Springer, 2011. 811~833
[51]  47 Labuhn I, Genty D, Daux V et al. Linking the isotopic composition of monthly precipitation, cave drip water and tree ring cellulose—15 years of monitoring and data-model comparison. EGU General Assembly Conference Abstracts, 2013, 15 :4818
[52]  48 刘忠方, 田立德, 姚檀栋等. 中国大气降水中 δ18O 的空间分布. 科学通报, 2009, 54 (6):804~811 Liu Zhongfang, Tian Lide, Yao Tandong et al. Spatial distribution of δ18O in precipitation over China. Chinese Science Bulletin, 2009, 54 (6):804~811
[53]  52 Zhao Liangju, Xiao Honglang, Zhou Maoxian et al. Factors controlling spatial and seasonal distributions of precipitation δ18O in China. Hydrological Processes, 2012, 26 (1):143~152

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