全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

树轮记录的小冰期以来青藏高原气候变化的时空特征

Keywords: 小冰期,青藏高原,温度变化,湿度变化,区域差异

Full-Text   Cite this paper   Add to My Lib

Abstract:

小冰期气候为评估现代气候变化提供了最直接的背景。本文主要依据树轮资料,同时结合现代仪器观测记录,利用经验正交函数(EOF)方法探讨了青藏高原小冰期以来气候变化的时空特征。首先分析了高原的温度变化。近50年来青藏高原的温度变化基本同相位变化,没有明显的区域差异;乌兰树轮序列是青藏高原的冬半年(9~4月)温度代用指标;利用6条指示夏季或暖季温度变化的树轮序列合并形成的新序列可指示高原春季-夏季(3~8月)温度变化;依据RCS(区域曲线标准化)方法建立的昌都树轮序列,能够反映整个青藏高原的年平均温度变化;不同季节的温度重建序列均显示17世纪和18世纪20~70年代是高原小冰期气候寒冷的时期,而18世纪初,19世纪后半叶,20世纪中期的气候较温暖,且均显示20世纪末期气候的快速增暖事实。其次,从重建的亚洲区域夏季PDSI(PalmerDroughtSeverityIndex)网格化数据集中提取42个网格点数据,分析了过去700年(1300~2005A.D.)高原的湿度变化。发现前3个特征向量代表了高原过去湿度变化的主要空间模态,与利用器测降水记录展开的EOF模态基本一致,表明主导高原干湿变化时空差异的物理过程是稳定的,不随时间而变化;近700年来高原南北部湿度变化具有明显的区域差异,最显著的差别是:自20世纪中期以来高原北部存在明显的变湿趋势,而高原南部却恰恰相反,呈现逐渐变干的趋势;近700年来高原南部的干湿变化有超前于高原北部的趋势。

References

[1]  Yang B, Kang X,Br?uning A et al.A 622-year regional temperature history of south east Tibet derived from tree rings.The Holocene,2010, 20 (2):181~190
[2]  Yang B, Kang X,Liu J et al.Annual temperature history in south west Tibet during the last 400 years recorded by tree rings.International Journal of Climatology,2010, 30 (7):962~971
[3]  Helle G, Schleser G,Br?uning A.Climate history of the Tibetan Plateau for the last 1500 years as inferred from stable carbon isotopes in tree-rings.In: Proceedings of the International Conference on the Study of Environmental Change Using Isotope Techniques,IAEA,2002.301~311
[4]  Cook E R, Anchukaitis K J,Buckley B M et al.Asian monsoon failure and megadrought during the last millennium.Science,2010, 328 :486~489
[5]  Lamb H H. Climate: Present,Past and Future.London: Methuen,1977.835
[6]  秦大河,陈宜瑜,李学勇.中国的气候与环境变化.北京: 科学出版社,2005.561
[7]  Qin Dahe,Chen Yiyu,Li Xueyong.The Chinese Climatic and Environmental Change.Beijing: Science Press,2005.561
[8]  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 浏览
[9]  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
[10]  Gou X, Chen F,Jacoby G et al.Rapid tree growth with respect to the last 400 years in response to climate warming,north eastern Tibetan Plateau.International Journal of Climatology,2007, 27 (11):1497~1503
[11]  Liang E, Shao X,Qin N.Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau.Global and Planetary Change,2008, 61 (3~4):313~320
[12]  Shao Xuemei,Fan Jinmei.Past climate on west Sichuan Plateau as reconstructed from ring-widths of Dragon Spruce.Quaternary Sciences,1999,(1):81~89
[13]  Fan Z X, Br?uning A,Yang B et al.Tree ring density-based summer temperature reconstruction for the central Hengduan Mountains in southern China.Global and Planetary Change,2009, 65 (1~2):1~11
[14]  Fan Z X, Br?uning A,Tian Q H et al.Tree ring recorded May-August temperature variations since AD 1585 in the Gaoligong Mountains,south eastern Tibetan Plateau.Palaeogeography,Palaeoclimatology,Palaeoecology,2010, 296 (1~2):94~102
[15]  Yang B, Br?uning A,Liu J et al.Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings.Global and Planetary Change,2009, 69 (1~2):71~78
[16]  Tan M, Liu T,Hou J et al.Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature.Geophysical Research Letters,2003, 30 (12):1617~1620
[17]  Ge Q S, Zheng J Y,Fang X Q et al.Winter half-year temperature reconstruction for the middle and lower reaches of the Yellow River and Yangtze River,China,during the past 2000 years.The Holocene, 13 (6):933~940
[18]  Liang E, Liu X,Yuan Y et al.The 1920s drought recorded by tree rings and historical documents in the semi-arid and arid areas of northern China.Climatic Change,2006, 79 (3):403~432
[19]  汤懋苍,许曼春.祁连山区的气候变化.高原气象,1984, 3 (4):21~33
[20]  Tang Maocang,Xu Manchun.Climatic variations of the Qilian Mountains.Plateau Meteorology,1984, 3 (4):21~33
[21]  汤懋苍,李存强,张 建.青藏高原及其四周的近代气候变化.高原气象,1988, 7 (1):39~49
[22]  Tang Maocang,Li Cunqiang,Zhang Jian.Mordern climatic change of Qinghai-Tibet Plateau and its surrounding regions. Plateau Meteorology,1988, 7 (1):39~49
[23]  Yao Tandong, Xie Zichu,Wu Xiaoling et al.Climatic change since Little Ice Age recorded by Dunde Ice Cap.Science in China(Series B),1991, 34 (6):760~767
[24]  Feng Song, Tang Maocang,Wang Dongmei.New evidence for the Qinghai-Xizang(Tibet)Plateau as a pilot region of climatic fluctuation in China.Chinese Science Bulletin,1998, 43 (6):633~636
[25]  Yang B, Qin C,Huang K et al.Spatial and temporal patterns of variations in tree growth over the north eastern Tibetan Plateau during the period AD 1450~2001.The Holocene,2010, 20 (8):1235~1245
[26]  王亚军,马玉贞,鲁瑞洁等.树木年轮记录的祁连山东段公元1895年来的气温变化.第四纪研究,2009, 29 (5):905~912 浏览
[27]  Wang Yajun,Ma Yuzhen,Lu Ruijie et al.Reconstruction of mean temperatures of January to August since A.D.1895 based on tree ring data in the eastern part of the Qilian Mountains.Quaternary Sciences,2009, 29 (5):905~912
[28]  刘 禹,田沁花,宋慧明等.以树轮宽度重建公元1558年以来华山5~6月平均温度及20世纪中后期升温.第四纪研究,2009, 29 (5):888~895 浏览
[29]  Liu Yu,Tian Qinhua,Song Huiming et al.Tree-ring width based May-June mean temperature reconstruction for Hua Mountains since AD 1558 and 20th century warming.Quaternary Sciences,2009, 29 (5):888~895
[30]  陈 峰,袁玉江,魏文寿等.福建沙县马尾松树轮宽度与夏季亚洲-太平洋涛动指数的关系.第四纪研究,2011, 31 (1):96~103 浏览
[31]  Chen Feng,Yuan Yujiang,Wei Wenshou et al.Correlations between the summer Asian Pacific Oscillation Index and the tree-ring width of Pinus massiniana from Sha County,Fujian Province.Quaternary Sciences,2011, 31 (1):96~103
[32]  马 龙,刘廷玺,冀鸿兰等.科尔沁沙地1826年以来榆树树轮宽度年表的建立及降水重建.第四纪研究,2011, 31 (2):360~369 浏览
[33]  Ma Long,Liu Tingxi,Ji Honglan et al.Establishment of ring width chronology and rainfall reconstruction of Ulmus pumila L. in Horqin sandy land since 1826.Quaternary Sciences,2011, 31 (2):360~369
[34]  靳立亚,秦宁生,勾晓华等.青海南部高原近450年来春季最高气温序列及其时变特征.第四纪研究,2005, 25 (2):193~201 浏览
[35]  Jin Liya,Qin Ningsheng,Gou Xiaohua et al.Series of spring maximum temperature in southern Qinghai Plateau and analysis of its variations during the last 450 years.Quaternary Sciences,2005, 25 (2):193~201
[36]  史江峰,鹿化煜,万建东等.采用华山松树轮宽度重建秦岭东缘近百年冬半年温度.第四纪研究,2009, 29 (4):831~836 浏览
[37]  Shi Jiangfeng,Lu Huayu,Wan Jiandong et al.Winter-half year temperature reconstruction of the last century using Pinus armandii franch tree-ring width chronology in the eastern Qinling Mountains.Quaternary Sciences,2009, 29 (4):831~836
[38]  Esper J, Cook E,Schweingruber F.Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability.Science,2002, 295 :2250~2253
[39]  Briffa K R, Shishov V V,Melvin T M et al.Trends in recent temperature and radial tree growth spanning 2000 years across north West Eurasia.Philosophical Transactions of the Royal Society B: Biological Sciences,2008, 363 :2269~2282
[40]  Mann M E, Zhang Z H,Hughes M K et al.Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia.Proceedings of the National Academy of Sciences of the United States of America, 2008, 105 (36):13252~13257
[41]  Kang Xingcheng,Graumlich L J,Sheppard P.The last 1835 years climate changes inferred from tree ring records in Dulan region,Qinghai,China.Quaternary Sciences,1997,(1):70~75
[42]  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 浏览
[43]  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
[44]  Shao X, Xu Y,Yin Z Y et al.Climatic implications of a 3585-year tree-ring width chronology from the north eastern Qinghai-Tibetan Plateau.Quaternary Science Reviews,2010, 29 (17~18): 2 111~2122
[45]  Zhang Q B, Cheng G,Yao T et al.A 2326-year tree-ring record of climate variability on the north eastern Qinghai-Tibetan Plateau.Geophysical Research Letters,2003, 30 (14):1739~1742
[46]  Sheppard P, Tarasov P,Graumlich L et al.Annual precipitation since 515 BC reconstructed from living and fossil juniper growth of north eastern Qinghai Province,China.Climate Dynamics,2004, 23 (7):869~881
[47]  Liu Y, An Z,Ma H et al.Precipitation variation in the north eastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the northern Hemisphere temperature.Science in China(Series D),2006, 49 (4):408~420
[48]  Liu Y, An Z S,Linderholm H W et al.Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings.Science in China (Series D),2009, 52 (3):348~359
[49]  刘晓宏,秦大河,邵雪梅等.祁连山中部过去近千年温度变化的树轮记录.中国科学(D辑),2004, 34 (1):89~95
[50]  Liu Xiaohong,Qin Dahe,Shao Xuemei et al.Tree-ring records of temperature change in the central Qilian Mountains in the past millennium.Science in China (Series D),2004, 34 (1):89~95
[51]  Liu X, Shao X,Zhao L et al.Dendroclimatic temperature record derived from tree-ring width and stable carbon isotope chronologies in the middle Qilian Mountains,China.Arctic,Antarctic,and Alpine Research,2007, 39 (4):651~657
[52]  Zhang Y, Tian Q,Gou X et al.Annual precipitation reconstruction since AD 775 based on tree rings from the Qilian Mountains,north western China.International Journal of Climatology,2011, 31 (3):371~381
[53]  Zhu H F, Zheng Y H,Shao X M et al.Millennial temperature reconstruction based on tree-ring widths of Qilian Juniper from Wulan,Qinghai Province,China.Chinese Science Bulletin,2008, 53 (24):3914~3920
[54]  Qin C, Yang B,Burchardt I et al.Intensified pluvial conditions during the twentieth century in the inland Heihe River Basin in arid North western China over the past millennium.Global and Planetary Change,2010, 72 (3):192~200
[55]  Yang B, Qin C,Shi F et al.Tree ring-based annual streamflow reconstruction for the Heihe River of arid north western China since AD 575 and its implication to water resources management.The Holocene,2012, 21 (7),in press.
[56]  Br?uning A. Dendrochronology for the last 1400 years in eastern Tibet.GeoJournal,1994, 34 (1):75~95
[57]  Br?uning A. Climate history of the Tibetan Plateau during the last 1000 years derived from a network of Juniper chronologies.Dendrochronologia,2001, 19 (1):127~137
[58]  Br?uning A, Mantwill B.Summer temperature and summer monsoon history on the Tibetan Plateau during the last 400 years recorded by tree rings.Geophysical Research Letters,2004, 31 (24), L24205,doi: 10.1029/2004GL020793
[59]  Br?uning A, Grieinger J.Late Holocene variations in monsoon intensity in the Tibetan-Himalayan region-evidence from tree rings.Journal of the Geological Science of India,2006, 68 (3):485~493
[60]  Fang K, Gou X,Chen F et al.Reconstructed droughts for the south eastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variability.Climate Dynamics,2010, 35 (4):577~585
[61]  Li Z S, Zhang Q B,Ma K.Tree-ring reconstruction of summer temperature for AD 1475~2003 in the Central Hengduan Mountains,north western Yunnan,China.Climatic Change,2011,doi: 10.1007/s10584-011-0111-z
[62]  Liang E, Shao X,Xu Y.Tree-ring evidence of recent abnormal warming on the south east Tibetan Plateau.Theoretical and Applied Climatology,2009, 98 (1):9~18
[63]  Liu J, Yang B,Qin C.Tree-ring based annual precipitation reconstruction since AD 1480 in south central Tibet.Quaternary International,2011, 236 (1~2):75~81
[64]  Wang X, Zhang Q B,Ma K et al.A tree-ring record of 500-year dry-wet changes in northern Tibet,China.The Holocene,2008, 18 (4):579~588
[65]  Wang S W, Gong D Y,Zhu J H.Twentieth-century climatic warming in China in the context of the Holocene.The Holocene,2001, 11 (3):313~321
[66]  Yang B, Br?uning A,Johnson K R et al.General characteristics of temperature variation in China during the last two millennia.Geophysical Research Letters,2002, 29 (9):381~384
[67]  Yang B, Br?uning A,Shi Y F.Late Holocene temperature variations on the Tibetan Plateau.Quaternary Science Reviews,2003, 22 (21~22):2335~2344
[68]  Yang B, Wang J,Br?uning A et al.Late Holocene climatic and environmental changes in arid Central Asia.Quaternary International,2009, 194 (1~2):68~78
[69]  Esper J, Schweingruber F H,Winiger M.1,300 years of climate history for western Central Asia inferred from tree-rings.The Holocene,2002, 12 (3):267~277
[70]  Liu X, Yin Z Y.Spatial and temporal variation of summer precipitation over the eastern Tibetan Plateau and the North Atlantic Oscillation.Journal of climate,2001, 14 (13):2896~2909 2.0.CO;2 target="_blank">
[71]  王可丽,江 灏,赵红岩.西风带与季风对中国西北地区的水汽输送.水科学进展,2005, 16 (3):432~438
[72]  Wang Keli,Jiang Hao,Zhao Hongyan.Atmospheric water vapor transport from westerly and monsoon over the North West China.Advances in Water Science,2005, 16 (3):432~438
[73]  Wang Y, Cheng H,Edwards R L et al.The Holocene Asian monsoon: Links to solar changes and North Atlantic climate.Science,2005, 308 :854~857
[74]  Hu C, Henderson G M,Huang J et al.Quantification of Holocene Asian monsoon rainfall from spatially separated cave records.Earth and Planetary Science Letters,2008, 266 (3~4):221~232
[75]  Zheng J, Wang W,Ge Q et al.Precipitation variability and extreme events in eastern China during the past 1500 years.Terrestrial Atmospheric and Oceanic Sciences,2006, 17 (3):579~592

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133