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地理学报 >

2013 , Vol. 68 >Issue 5: 579 - 592

DOI: https://doi.org/10.11821/xb201305001

气候变化

过去2000年冷暖变化的基本特征与主要暖期

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  • 1. 中国科学院地理科学与资源研究所, 北京 100101;
    2. 南京师范大学地理科学学院, 南京 210023;
    3. 中国科学院南京地理与湖泊研究所, 南京 210008;
    4. 北京师范大学地理学与遥感科学学院, 北京 100875;
    5. 中国科学院寒区旱区环境与工程研究所, 兰州 730000
葛全胜(1963- ), 男, 安徽安庆人, 研究员, 中国地理学会会员(S110000942M), 从事全球变化研究。E-mail: geqs@igsnrr.ac.cn

收稿日期: 2013-01-31

  修回日期: 2013-03-28

  网络出版日期: 2013-05-20

基金资助

国家重点基础研究发展计划项目(2010CB950100);中国科学院战略性先导科技专项项目(XDA05080100);科技基础性工作专项项目(2011FY120300)

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General characteristics of temperature change and centennial warm periods during the past 2000 years

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  • 1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
    2. School of Geography, Nanjing Normal University, Nanjing 210023, China;
    3. Nanjing Institute of Geography and Limnology, CAS, Nanjing 210008, China;
    4. School of Geography, Beijing Normal University, Beijing 100875, China;
    5. Institute of Cold and Arid Regions Environmental and Engineering, CAS, Lanzhou 730000, China

Received date: 2013-01-31

  Revised date: 2013-03-28

  Online published: 2013-05-20

Supported by

China Global Change Research Program, No.2010CB950100; The "Strategic Priority Research Program" of the Chinese Academy of Sciences, No. XDA05080100; Basic Research Project of the Ministry of Science and Technology, No.2011FY120300

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摘要

根据近年国内外相关研究结果,分析了北半球与中国过去2000 年冷暖变化的阶段性,辨识了百年尺度暖期的起讫年代及其与20 世纪温暖程度的差别。结果表明:(1) 最近新建的多数北半球温度变化序列显示公元1-270 年温暖;271-840 年冷暖相间,但总体偏冷;841-1290年温暖;1291-1910 年寒冷;1911 年以后再次转为温暖;这些冷暖阶段虽分别与Lamb 指出的罗马暖期(约公元前1 世纪-4 世纪中期)、黑暗时代冷期(约4 世纪末-10 世纪前期)、中世纪暖期(约10 世纪中期-13 世纪末)、小冰期(约15-19 世纪) 以及20 世纪增暖大致对应,但各阶段的起讫时间与Lamb确定的时段存在一定差别。(2) 尽管过去2000 年冷暖变化过程及其变幅大小在中国境内各个区域间并不完全一致,但从全国平均看,中国与北半球百年尺度的冷暖波动阶段基本一致,仅起讫年代存在一定差异;其中公元1-200 年、551-760 年、941-1300 年及20世纪气候相对温暖,其他时段则相对寒冷。(3) 多数序列显示中世纪期间北半球的温暖程度至少与20 世纪相当。中国941-1300 年间的最暖百年和最暖30 年(暖峰) 的温度也略高于20 世纪,551-760 年间的最暖百年与20 世纪基本相当,但1-200 年间最暖百年的温暖程度则较20 世纪略低。

关键词： 过去2000年; 北半球; 中国; 温度变化; 百年际暖期

本文引用格式

葛全胜, 刘健, 方修琦, 杨保, 郝志新, 邵雪梅, 郑景云 . 过去2000年冷暖变化的基本特征与主要暖期[J]. 地理学报, 2013 , 68(5) : 579 -592 . DOI: 10.11821/xb201305001

Abstract

The characteristics of warm/cold fluctuation for Northern Hemisphere (NH) and China during the past 2000 years were analyzed using the proxy-based temperature change series published recently. The duration of centennial warm periods before the 20th century and the difference between the warmth of the 20th century and the centennial warm periods that occurred prior to the 20th century were also investigated. The conclusions are summarized as follows: (1) Most of proxy-based NH temperature series show that the warm climate occurred in the periods of AD 1-270, 841-1290 and 1911-2000. In general, it was cool with multi-decadal temperature fluctuations from 271 to 840, and cold from 1291 to 1910. These centennial periods of warm/cold fluctuation over NH are corresponding to the Roman Warm Period (the 1st century BC to the mid-4th century AD), Dark Age Cold Period (the end of 4th century to the early of 10th century AD), Medieval Warm Period (the mid-10th century to the end of 13th century AD), Little Ice Age (the 15th to 19th century) and Warming Period in the 20th century illustrated by Lamb respectively. But they have different durations between the NH centennial warm/cold periods and those Warm/Cold Periods identified by Lamb. (2) The duration and amplitude of regional centennial phases of warm/cold fluctuation are different in China, but the timing of centennial periods of warm/cold over whole China, i.e. warm in AD 1-200, 551-760, 941-1300, 1901-2000 and cold in the others, which are consistent with that observed in NH approximately. (3) Most of proxy-based NH temperature change series show that the warmth in Medieval Warm Period is at least comparable to that during the Warming Period in the 20th century. The warmest 100-year and 30-year (i.e., warm peak duration) for whole China occurred in the periods of 941-1300 during the past 2000 years, which are slightly higher than in the 20th century respectively. Moreover, the temperature anomalies in the warmest 100-year and 30-year for whole China that occurred in the periods of 571-760 and 1-200 are comparable to and a little lower in the 20th century respectively.

Key words： temperature change; centennial warm period; the past 2000 years; Northern Hemisphere; China

参考文献

[1] PAGES. Science Plan and Implementation Strategy. IGBP Report No.57. IGBP Secretariat, Stockholm. 2009. 67pp.

[2] Hughes M K, Diaz H F. Was there a medieval warm period, and if so, where and when? Climatic Change, 1994, 26 (2-3): 109-142.

[3] Diaz H F, Trigo R, Hughes M K et al. Spatial and temporal characteristics of climate in Medieval Times revisited. Bulletin of the American Meteorological Society, 2011, 92: 1487-1500.

[4] Ge Q S, Zheng J Y, Hao Z X et al. General characteristics of climate changes during the past 2000 years in China. Science in China Series D: Earth Sciences, 2012, doi: 10.1007/s11430-012-4370-y.

[5] Ge Quansheng, Zheng Jingyun. Progress on the study of the forcing and impacts of the warm periods in China during the past 2000 years. Geographical Research, 2012, 31(4): 769.[葛全胜, 郑景云. 过去2000 年全球典型暖期的形成机制 及其影响研究进展. 地理研究, 2012, 31(4): 769.]

[6] Brooks C E P. The Evolution of Climate. London: Benn Brothers, 1922, 173pp.

[7] Lamb H H. The early medieval warm epoch and its sequel. Palaeogeography, Palaeoclimatology, Palaeoecology, 1965, 1 (1): 13-37.

[8] Lamb H H. Climate: Present, Past and Future. Vol. 2: Climatic History and the Future. London: Methuen, 1977, 837pp.

[9] Patterson W P. Stable isotopic record of climatic and environmental change in continental settings[D]. University of Michigan, 1995.

[10] Bianchi G G, McCave I N. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland. Nature, 1999, 397: 515-517.

[11] Patterson W P, Dietrich KA, Holmden C et al. Two millennia of North Atlantic seasonality and implications for Norse colonies. Proceedings of the National Academy of Sciences of the United States of America 2010, 107(12): 5306-5310, doi: 10.1073/pnas.0902522107.

[12] IPCC. Climate Change: The IPCC Scientific Assessment. Houghton J, Jenkins G J, Epharums J J eds. Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press, 1990: 201-205.

[13] Bradley R S, Jones P D. "Little Ice Age" summer temperature variations: Their nature and relevance to recent global warming trends. The Holocene, 1993, (3): 367-376.

[14] Jones P D, Mann M E. Climate over past millennia. Reviews of Geophysics, 2004, 42(2): 1-42.

[15] Jones P D, Briffa K R, Osborn T J et al. High-resolution palaeoclimatology of the last millennium: A review of current status and future prospects. The Holocene, 2009, 19(1): 3-49.

[16] IPCC. Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Solomon S, Qin D, Manning M et al eds. Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press, 2007: 466-482.

[17] Mann M E, Bradley R S, Hughes M K. Northern hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations. Geophysical Research Letters, 1999, 26(6): 759-762.

[18] Mann M E, Jones P D. Global surface temperatures over the past two millennia. Geophysical Research Letters, 2003, 30(15): 1820, doi: 10.1029/2003GL017814.

[19] Briffa K R. Annual climate variability in the Holocene: Interpreting the message of ancient trees. Quaternary Science Reviews, 2000, 19: 87-105.

[20] Briffa K R, Osborn T J, Schweingruber F H. Large-scale temperature inferences from tree rings: A review. Global Planet Change, 2004, 40: 11-26.

[21] Jones P D, Briffa K R, Barnett T P et al. High resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with general circulation model control-run temperatures. The Holocene, 1998, 8(4): 455-471.

[22] Jones P D, Osborn T J, Briffa K R. The evolution of climate over the last millennium. Science, 2001, 292: 662-667.

[23] Hegerl G C, Crowley T J, Hyde W T et al. Climate sensitivity constrained by temperature reconstructions over the past seven centuries. Nature, 2006, 440: 1029-1032.

[24] Esper J, Cook E R, Schweingruber F H. Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science, 2002, 295: 2250-2253.

[25] Cook E R, Esper J, D'Arrigo R. Extra-tropical Northern Hemisphere land temperature variability over the past 1000 years. Quaternary Science Reviews, 2004, 23(20-22): 2063-2074.

[26] D'Arrigo R, Wilson R, Jacoby G. On the long-term context for late twentieth century warming. J. Geophys. Res., 2006, 111(D3), doi: 10.1029/2005JD006352.

[27] Moberg A, Sonechkin D M, Holmgren K et al. Highly variable Northern Hemisphere temperatures reconstructed from low-and high-resolution proxy data. Nature, 2005, 433: 613-617.

[28] Bradley R S, Hughes M K, Diaz H F. Climate in Medieval Time. Science, 2003, 302: 404-405, doi: 10.1126/science.1090372.

[29] Osborn T J, Briffa K R. The spatial extent of 20th-century warmth in the context of the past 1200 years. Science, 2006, 311: 841-844.

[30] Soon W, Baliunas S, Idso C et al. Reconstructing climatic and environmental changes of the past 1000 years: Reappraisal. Energy & Environment, 2003, 14(2/3): 233-296.

[31] Loehle C. A 2000-year global temperature reconstruction based on non-tree ring proxies. Energy & Environment, 2007, 18: 1049-1058.

[32] Loehle C, McCulloch J H. Correction to: A 2000-year global temperature reconstruction based on non-tree ring proxies. Energy & Environment, 2008, 19: 93-100.

[33] Mann M E, Zhange 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: 13252-13257.

[34] Mann M E, Zhange Z H, Rutherford S et al. Global signatures and dynamical origins of the Little Ice Age and medieval climate anomaly. Science, 2009, 326(5957): 1256-1260.

[35] Ljungqvist F C. A new reconstruction of temperature variability in the extra-tropical Northern Hemisphere during the last two millennia. Geografiska Annaler: Series A, Physical Geography, 2010, 92(3): 339-351.

[36] Mcshane B B, Wyner A J. A statistical analysis of multiple temperature proxies: Are reconstructions of surface temperatures over the last 1000 years reliable. Annals of Applied Statistics, 2011, 5(1): 5-44.

[37] Christiansen B, Ljungqvist F C. The extra-tropical Northern Hemisphere temperature in the last two millennia: Reconstructions of low-frequency variability. Climate of the Past, 2012, 8(2): 765-786.

[38] Wanner H, Beer J, Bütikofer J et al. Mid-to late Holocene climate change: An overview. Quaternary Science Reviews, 2008, 27: 1791-1828.

[39] Bürger G. On the verification of climate reconstructions. Climate of the Past, 2007, 3: 397-409.

[40] Christiansen B, Schmith T, Thejll P. A surrogate ensemble study of climate reconstruction methods: Stochasticity and robustness. Journal of Climate, 2009, 22(4): 951-976.

[41] Chu Ko-chen. A preliminary study on the climatic fluctuations during the last 5000 years in China. Acta Archaeologica Sinica, 1972, (1): 15-38.[竺可桢. 中国近五千年来气候变迁的初步研究. 考古学报, 1972, (1): 15-38.]

[42] Zhang Piyuan, Gong Gaofa. Some characteristics of climatic fluctuations in China since the 16th century. Acta Geographica Sinica, 1979, 34(3): 238-247.[张丕远, 龚高法. 1979. 16 世纪以来中国气候变化的若干特征. 地理学报, 1979, 34(3): 238-247.]

[43] Zhang Piyuan. Climate Changes in China during Historical Times. Jinan: Shandong Science & Technology Press, 1996: 195-440.[张丕远. 中国历史气候变化. 济南: 山东科学技术出版社, 1996: 195-440.]

[44] Zhang D E. Winter temperature changes during the last 500 years in South China. Chinese Science Bulletin, 1980, 25 (6): 497-500.

[45] Zheng Sizhong. Climate and its effect on food production during the Little Ice Age in Guangdong Province. Chinese Science Bulletin, 1982, 27(10): 1081-1084.

[46] Wang S W, Wang R S. Reconstruction of temperature series of North China from 1380s to 1980s. Science in China: Series B, 1991, (6): 751-759

[47] Wang Shaowu, Wang Risheng. Variations of seasonal and annual temperatures during 1470-1978AD in eastern China. Acta Meteorologica Sinica, 1990, 48(1): 26-35.[王绍武, 王日昇. 1470 年以来我国华东四季与年平均温度变化的研 究. 气象学报, 1990, 48(1): 26-35.]

[48] Ge Quansheng, Zheng Jingyun, Fang Xiuqi et al. Reconstruction and analysis on the series of winter-half-year temperature changes over the past 2 000 years in eastern China. Earth Science Frontiers, 2002, 9(1): 169-181.[葛全 胜, 郑景云, 方修琦等. 过去2000a中国东部冬半年温度变化序列重建及初步分析. 地学前缘, 2002, 9(1): 169-181.]

[49] Shao Xuemei, Wu Xiangding. Reconstruction of climate change on Changbai Mountain, Northeast China using tree-ring data. Quaternary Sciences, 1997, (1): 77-85.[邵雪梅,吴祥定. 利用树轮资料重建长白山区过去气候变化. 第四纪研究, 1997, (1): 77-85.]

[50] Shao Xuemei, Fan Jinmei. Past climate on west Sichuan Plateau as reconstructed from ring-widths of dragon spruce. Quaternary Sciences, 1999, (1): 81-89.[邵雪梅, 范金梅. 树轮宽资料所指示的川西过去气候变化. 第四纪研究, 1999, (1): 81-89.]

[51] Liu Xiaohong, Qin Dahe, Shao Xuemei et al. Temperature variations recovered from tree-rings in the middle Qilian Mountain over the last millennium. Science in China Series D: Earth Sciences, 2005, 48(4): 521-529.

[52] Zhu H F, Zheng Y H, Shao X M et al., Millennial temperature reconstruction based on treering widths of Qilian juniper from Wulan, Qinghai Province, China. Chinese Science Bulletin, 2008, 53: 3914-3920.

[53] Shao X M, Xu Y, Yin Z Y et al. Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai-Tibetan Plateau. Quaternary Science Reviews, 2010, 29: 2111-2122, doi: 10.1016/j. quascirev.2010.05.005.

[54] Xu Qinghai, Xiao Jule, Toshio Nakamura et al. Climate changes of Daihai basin during the past 1 500 from a pollen record. Quaternary Sciences, 2004, 24(3): 341-347.[许清海, 肖举乐, 中村俊夫等. 2004. 孢粉记录的岱海盆地1500 年以来气候变化. 第四纪研究, 2004, 24(3): 341-347.]

[55] Yao T D, Qin D H, Xu B Q et al. Temperature change over the past millennium recorded in ice cores from the Tibetan Plateau. Advances in Climate Change Research, 2006, 2(3): 99-103.[姚檀栋, 秦大河, 徐柏青等. 2006. 冰芯 记录的过去1000a青藏高原温度变化. 气候变化研究进展, 2006, 2(3): 99-103.]

[56] Thompson L G, Thompson E M, Brecher H et al. Abrupt tropical climate change: Past and present. Proceedings of the National Academy of Sciences of the United States of America, 2006, 103: 10536-10,543

[57] Wang N L, Yao T D, Pu J C et al. Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau. Science in China Series D: Earth Sciences, 2006, 49(10): 1079-1089.

[58] Tan M, Liu T S, Hou J Z et al. Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature. Geophysical Research Letters, 2003, 30(20): 1617, doi: 10.1029/2003GL017352.

[59] Shen Ji, Zhang Eenlou, Xia Weilan. Records from lake sediments of the Qinghai Lake to mirror climatic and environmental changes of the past about 1000 year. Quaternary Sciences, 2001, 21(6): 508-513.[沈吉, 张恩楼, 夏威 岚. 青海湖近千年来气候环境变化的湖泊沉积记录. 第四纪研究, 2001, 21(6): 508-513.]

[60] Liu Z H, Henderson A C G, Huang Y S. Alkenone-based reconstruction of late-Holocene surface temperature and salinity changes in Lake Qinghai, China. Geophysical Research Letters, 2006, 33: L09707, doi: 10.1029/2006GL026151.

[61] Chu G Q, Sun Q, Wang X H et al. Seasonal temperature variability during the past 1600 years recorded in historical documents and varved lake sediment profiles from northeastern China. The Holocene, 2012, 22: 785-792

[62] Wang S W, Gong D Y. Climate in China during the four special periods in Holocene. Progress in Natural Science, 2000, 10(5): 379-386.

[63] Ge Quansheng, Fang Xiuqi, Zheng Jingyun. Warm-cold change in millenarian cycle derived from natural proxy data in china during the past 3000 years. Advance in Earth Sciences, 2002, 17(1): 96-103.[葛全胜, 方修琦, 郑景云. 中国过 去3ka冷暖千年周期变化的自然证据及其集成分析. 地球科学进展, 2002, 17(1): 96-103.]

[64] Yang Bao, Braeuning 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

[65] Ge Q S, Wang S B, Zheng J Y. Reconstruction of temperature series in China for the last 5000 years. Progress in Natural Science, 2006, 16(8): 838-845.

[66] Ge Quansheng. The Climate Change in China during the Past Dynasties. Beijing: Science Press, 2011, 705pp.[葛全 胜. 中国历朝气候变化. 北京: 科学出版社, 2011: 705pp.

[67] Ge Quansheng, Zheng Jingyun, Hao Zhixin et al. Temperature variation through 2000 years in China: An uncertainty analysis of reconstruction and regional difference. Geophysical Research Letters, 2010, 37: L03703, doi: 10.1029/2009GL041281.

[68] Hong Y T, Liu D S, Jiang H B et al. Evidence for solar forcing of climate variation from δ18O of peat cellulose. Science in China: Series D Earth Sciences, 2000, 43(2): 217-224.

[69] Holmes J A, Zhang J W, Chen F H et al. Paleoclimatic implications of an 850-year oxygen-isotope record from the northern Tibetan Plateau. Geophysical Research Letters, 2007, 34: L23403, doi: 10.1029/2007GL032228.

[70] Tang Guoli, Ding Yihui, Wang Shaowu et al. Comparative analysis of the time series of surface air temperature over China for the last 100 years. Advances in Climate Change Research, 2009, 5(2): 71-78.[唐国利, 丁一汇, 王绍武等. 中国近百年温度曲线的对比分析. 气候变化研究进展, 2009, 5 (2): 71-78.]

[71] Hoskuldsson A. PLS regression methods. Journal of Chemometrics, 1988, 2: 211-228.
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