收稿日期: 2008-10-15
修回日期: 2009-01-06
网络出版日期: 2009-02-10
基金资助
中国科学院知识创新工程重要方向项目“过去2000年东亚季风气候演变及其与人类相互作用研究”(编号:KZCX2-YW-315);国家自然科学基金项目“近千年来东亚季风年代—世纪尺度变化的模拟与重建资料综合研究”(编号:40672210);“中国东部近千年来土地利用变化对东亚季风气候影响的模拟研究”(编号:40871007)共同资助.
Comparison of Simulated and Reconstructed Precipitation in China during the Last Millennium
Received date: 2008-10-15
Revised date: 2009-01-06
Online published: 2009-02-10
依据中国区域27年GPCP降水观测再分析资料、500年旱涝等级资料及近千年冰芯、树轮、湖芯等降水代用资料,对全球海气耦合气候模式ECHO-G近千年积分模拟降水进行时空变化的对比分析,检验模式对中国地区降水的模拟性能。结果表明模拟降水较好体现了中国区域降水年平均和季节平均的分布型态,并在年代际变化上与历史记录一致。中国西部模拟降水呈现出与重建资料一致的准200年的百年际周期及20~30年左右的年代际周期,并与湖泊盐度的高低时段对应较好。总体而言,模式成功再现了观测及代用资料所体现的中国区域近千年降水的主要时空变化特征。EOF分析结果进一步揭示了3个不同气候特征时期模拟降水存在不同的区域分异特点。
况雪源 , 王红丽 , 王苏民 , 提汝媛 , 刘健 . 近千年来中国区域降水模拟与重建资料的对比分析[J]. 地球科学进展, 2009 , 24(2) : 159 -171 . DOI: 10.11867/j.issn.1001-8166.2009.02.0159
With more and more effects of human activities on natural climate variability, the climate change has becomes more complex in the past 1 000 years, which is the key period for linking the proxy data and instrumental observation periods. Aimed to the scarcity of observation and uncertainty of reconstructed proxy data in this period, climate model is developed as a useful tool for studying paleoclimate. ECHO-G is one of such advanced climate models, but its performance in simulating the rainfall in China has not been examined. In this paper, the datasets of 27 years′ observed precipitation reanalysis data of GPCP in China,500 years′ classified drought and flood data,and proxy data like ice core, tree-ring, lake sediment during the past 1000 years are chosen to examine the performance of the atmosphere-ocean coupled model ECHO-G in simulating precipitation in China. The comparison between GPCP reanalysis and simulated precipitation in each season shows the model well reproduced the spatial distributions of precipitation in China; and the comparison with 500 years′ classified drought and flood data indicates the simulation is in good consistent with the precipitation classification in interdecadal time scale. It is prone to be flood when there is more simulated precipitation, and drought when there is less simulated precipitation. Furthermore, both the simulated and tree-ring reconstructed precipitation show there exit inter-centennial cycle of quasi-200 year and inter-decadal oscillation of 20~30 year, i.e. the simulation well reflects the inter-decadal and inter-centennial variations of precipitation. Compared with the lake sediment, the period with more simulate precipitation is corresponding to low lake salinity, vice versa.. In total, simulated results successfully reflect the main temporal and spatial variations of precipitation in China during the last millennium. Furthermore, the EOF analysis reveals there exit different regional differentiation characteristics in simulated precipitation of three different typical climate periods.
Key words: Last millennium; China; Simulated precipitation; Reconstructed data
[1] Wang S. Climatic variations during the last millennium[M]//Ye Duzheng, Leng Qingcun, Wu Guoxiong,et al. eds. Climate, Environment and Geophysical Fluid Dynamics. Beijing: China Meteorological Press, 1993: 56-63.
[2] Ge Quansheng, Zheng Jingyun, Fang Xiuqi, et al. Temperature changes of winter-half-year in eastern China during the past 2000 years[J].Quaternary Sciences, 2002,22(2):166-173.[葛全胜,郑景云,方修琦,等.过去2000年中国东部冬半年温度变化[J]. 第四纪研究, 2002, 22(2):166-173.]
[3] Yang Bao,Achim Braeuning, Kathleen R Johnson. General characteristics of temperature variation in China during the last two millennia[J].Geophysical Research Letters, 2002, 29(9):1324.
[4] Wang Shaowu, Wen Xinyu, Luo Yong, et al. Reconstruction of temperature series in China during the last millennium[J].Chinese Science Bulletin, 2007,52(8):958-964.[王绍武,闻新宇,罗勇,等.近千年中国温度序列的建立[J]. 科学通报,2007,52(8):958-964.]
[5] Wang Shaowu, Xie Zhihui, Cai Jingning, et al. Study on variation of the global mean temperature during the last millennium[J].Progress in Natural Science, 2002,12(11):1 145-1 149.[王绍武,谢志辉,蔡静宁,等.近千年全球平均气温变化的研究[J].自然科学进展,2002,12(11):1 145-1 149.]
[6] Wang Shaowu, Luo Yong, Wen Xinyu, et al. Latest advances in studies of the global temperature variations for the last millennium[J].Advances in Climate Change Research, 2007,3(1):14-19.[王绍武,罗勇,闻新宇,等.近千年全球温度变化研究的新进展[J].气候变化研究进展,2007,3(1):14-19.]
[7] Liu Xiaohong, Qin Dahe, Shao Xuemei, et al. Tree-ring records of temperature change in the central Qilian Mountains in the past millennium[J]. Science in China(Series D),2004,34(1):89-95.[刘晓宏,秦大河,邵雪梅,等.祁连山中部过去千年温度变化的树轮记录[J]. 中国科学:D辑,2004,34(1):89-95.]
[8] Kang Xingcheng, Zhang Qihua. Reconstruction and variation of climate in Dulan region, Qinghai during last 2 000 years[J]. Advances in Earth Science, 2000,15(2):215-221.[康兴成,张其花. 青海都兰过去2000年来的气候重建及其变迁[J]. 地球科学进展,2000,15(2):215-221.]
[9] Shi Yafeng, Yao Tandong, Yang Bao. Decadal climatic variations recorded in Guliya ice core and comparison with historical documentary data from east China during the last 2 000 years[J]. Science in China (Series D), 1999, 29 (suppl.1): 79-86.[施雅风,姚檀栋,杨保. 近2 000年古里雅冰芯10年尺度的气候变化及其与中国东部文献记录的比较[J]. 中国科学:D辑,1996,29(增刊1):79-86.]
[10] Yao Tandong, Xu Boqing, Duan Keqin, et al. Temperature and methane records over the last 2ka in Tibetan Dasuopu ice core[J].Science in China(Series D), 2002,32(4):346-352.[姚檀栋,徐柏青,段克勤,等. 青藏高原达索普冰芯2ka来温度与甲烷浓度变化记录[J]. 中国科学:D辑,2002,32(4):346-352.]
[11] Zhang Deer, Liu Chuanzhi, Jiang Jianmin. Reconstruction-of six regional dry/wet series and their abrupt changes during the last 1000 years in east China[J].Quaternary Sciences,1997,17(1):1-11.[张德二,刘传志,江剑民. 中国东部6区域近1000年干湿序列的的重建和气候跃变分析[J]. 第四纪研究,1997,17(1):1-11.]
[12] Zhang Deer, Liu Yuewei, Liang Youye, et al. Reconstruction of annual and seasonal precipitation series of Nanjing, Suzhou and Hangzhou during the 18th century[J]. Quaternary Sciences,2005,25(2):121-128.[张德二,刘月巍,梁有叶,等. 18世纪南京、苏州和杭州年、季降水量序列的复原研究[J]. 第四纪研究,2005,25(2):121-128.]
[13] Zhang Peiyuan, Ge Quansheng, Zhang Shihuang, et al. The modes and abrupt changes of climate in China during recent 2000 years[J].Quaternary Sciences,1997,17(1):12-20.[张丕远,葛全胜,张时煌,等.2000年来我国旱涝气候演化的阶段性和突变[J]. 第四纪研究,1997,17(1):12-20.]
[14] Zheng Jingyun, Zhang Peiyuan, Ge Quansheng, et al. Inter-centennial variations of dry and wet changes in eastern China during the past 2000 years[J].Progress in Natural Science,2001,11(1):65-70.[郑景云,张丕远,葛全胜,等.过去2000年中国东部干湿分异的百年际变化[J]. 自然科学进展,2001,11(1):65-70.]
[15] Academy of Meteorological Science of the Central Meteorological Bureau. Precipitation Distribution Maps in China in recent 500 Years[M]. Beijing:SinoMaps Press,1981:320-332.[中央气象局气象科学研究院.中国近五百年旱涝分布图集[M]. 北京:地图出版社,1981:320-332.]
[16] Duan Keqin, Yao Tandong, Pu Jianchen. Precipatation variation recorded in a HimalayanIce core and its response to Tibetan temperature[J].Journal of Glaciology and Geocrylogy,2001,23(2):119-125.[段克勤, 姚檀栋,蒲健辰. 喜马拉雅山达索普冰川积累量变化及其对青藏高原温度的响应[J]. 冰川冻土,2001,23(2):119-125.]
[17] Shao Xuemei, Huang Lei, Liu Hongbin. Thousand year’s precipitation variation in Delingha, Qinghai based on tree-ring records[J].Science in China (Series D), 2004,34(2):145-153.[邵雪梅,黄磊,刘洪滨. 树轮记录的青海德令哈地区千年降水变化[J]. 中国科学:D辑,2004,34(2):145-153.]
[18] Shen Ji, Zhang Enlou, Xia Weilan. Reconstructions from lake sediments of the Qinghai Lake to mirror climatic and environmental changes of the past about 1000 years[J].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[J]. 第四纪研究,2001,21(6):508-513.]
[19] Zhou Tianjun, Yu Rucong. Twentieth century surface air temperature over China and the globe simulated by coupled climate models[J].Journal of Climate, 2006, 19(22): 5 843-5 858.
[20] Zorita E, Gonz lezRouco J F, von Storch H, et al. Natural and anthropogenic modes of surface temperature variations in the last thousand years[J].Geophysical Research Letters,2005, 32, L08707, doi:10.1029/2004GL021563.
[21] Legutke S, Voss R. The Hamburg Atmosphere-Ocean Coupled Circulation Model ECHO-G[R].Technical Report No.18.Hamburg, Germany:German Climate Computer Center (DKRZ), 1999.
[22] Baquero-Bernal A, Latif M, Legutke S. On dipole-like variability of sea surface temperature in the tropical Indian Ocean[J]. Journal of Climate,2002, 15(11): 1 358-1 368.
[23] Marsland S J, Latif M, Legutke S. Variability of the Antarctic circumpolar wave in a coupled ocean-atmosphere model[J]. Ocean Dynamics, 2003, 53(4): 323-331.
[24] Gonzalez-Ruoco F, von Storch H, Zorita E. Deep soil temperature as proxy for surface air-temperature in a coupled model simulation of the last thousand years[J].Geophysical Research Letters, 2003, 30(21): 2116.
[25] Raible C , Luksch U, Fraedrich K, et al. North Atlantic decadal regimes in a coupled GCM simulation[J].Climate Dynamics, 2001, 18: 321-330.
[26] Liu Jian, von Storch H, Chen Xing, et al. Simulated and reconstructed winter temperature in the eastern China during the last millennium[J].Chinese Science Bullentin,2005,50(24): 2 872-2 877.[刘健, von Storch H, 陈星,等. 千年气候模拟与中国东部温度重建序列的比较研究[J]. 科学通报, 2005, 50(20): 2 251-2 255.]
[27] Liu Jian, Gao Jianhui, Wang Sumin. Modeling study on the temperature changes in medieval warm period[J].Lake Science, 2006, 18(2): 97-105.[刘健, 高建慧, 王苏民. 中世纪暖期温度变化的模拟研究[J]. 湖泊科学, 2006, 18(2): 97-105.]
[28] Jian Liu, Hans von Storch, Eduardo Zorita,et al. Simulated and reconstructed temperature in China since 1550 AD[J].History of Meteorology,2005,2:87-104.
[29] Usoskin I, Solanki S, Schüessler M, et al. A millennium-scale sunspot number reconstruction: Evidence for an unusual active sun since the 1940s[J].Physical Review Letters,2003, 91: 2 114-2 116.
[30] Robock A, Free M. The volcanic record in ice cores for the past 2000 years[C]//Jones P, Bradley R, Jouzel J, eds. Climatic Variation and Forcing Mechanisms of the Last 2000 Years. New York: Springer-Verlag, 1996: 533-546.
[31] Etheridge D, Steele L P, Langenfelds R L, et al. Morgan Natural and anthropogenic changes in atmospheric CO2 over the last 1000 years from air in Antarctic ice and firn[J].Journal of Geophysical Research,1996, 101: 4 115-4 128.
[32] Blunier T, Chappellaz J A, Schwander J, et al. Variations in atmospheric methan concentration during the Holocene epoch[J]. Nature,1995, 374: 46-49.
[33] Phillip A Arkin,Pingping Xie.The global precipitation climatology project:First algorithm intercomparison project[J].Bulletin American Meteorological Society,1994,75(3):401-419.
[34] Robert F A,George J H,Alfred Chang,et al. The version-2 global precipitation climatology project (GPCP) monthly precipitation analysis (1979-present)[J].Journal of Hydrometeorology,2003, 4:1 147-1 167.
[35] Zhang Deer, Liu Chuanzhi. Additions to precipitation cistribution maps in China in recent 500 years(1980-1992)[J]. Meteorology, 1993, 19(11): 41-45.[张德二,刘传志. 中国近500年旱涝分布图集续补(1980—1992)[J].气象,1993, 19(11):41-45.]
[36] Yao Tandong, Qin Dahe, Tian Lide. Variations of Temperature and rainfall in Tibetan Plateau—Records of Guliya ice core[J]. Science in China (Series D),1996,26(4):348-353.[姚檀栋,秦大河,田立德. 青藏高原2ka来温度与降水变化——古里雅冰芯记录[J]. 中国科学:D辑,1996,26(4):348-353.]
[37] Zhang Enlou, Shen Ji, Wang Sumin, et al. Quantitative reconstruction of Qinghai lake salinity during the past 0.9ka[J].Chinese Science Bulletin,2004,49(7):697-701.[张恩缕,沈吉,王苏民,等. 近0.9ka来青海湖湖水盐度的定量恢复[J]. 科学通报,2004,49(7):697-701.]
[38] Zheng Jingyun, Hao Zhixin, Ge Quansheng. Seasonal precipitation reconstruction and analysis in Shandong province derived from the Archives in the Qing Dynasty since 1736[J].Climatic and Environmental Research,2004,9(4):551-566.[郑景云,郝志新,葛全胜. 山东1736年来逐季降水重建及其初步分析[J]. 气候与环境研究\[J\]. 2004,9(4):551-566.]
[39] Chen W Y. Fluctuations in Northern Hemisphere 700mb Height Field associated with the Southern Oscillation[J].Monthly Weather Review,1982,110:808-823.
[40] Yang Bao, Shi Yafeng.Comparison of Guliya ice core accumulation with other proxy precipitation data of China during the last two millennium[J].Marine Geology & Quaternary Geology,2001,21(3):61-66.[杨保,施雅风. 近2000年古里雅冰心积累量与中国其它地区降水代用资料的比较[J]. 海洋地质与第四纪地质,2001,21(3):61-66.]
[41] Xu Guochang, Yao Hui, Li Xinmin,et al. Climate Change in Arid and Semi-arid Areas in China\[M\]. Beijing: Meteorological Press, 1997:101.[徐国昌,姚辉,李新敏,等.中国干旱半干旱区气候变化[M]. 北京:气象出版社,1997:101.]
[42] Wang Shaowu, Cai Jingning, Mu Qiaozhen. Cliamte change of annual precipitations in western China[J].Journal of Natural Resources,2002,17(4):415-422.[王绍武,蔡静宁,慕巧珍.中国西部年降水量的气候变化[J]. 自然资源学报,2002,17(4):415-422.]
[43] Kuang Xueyuan, Liu Jian, Wang Hongli, et al. Inter-hemispheric comparison of climate change in the last millennium based on the ECHO-G simulation[J].Chinese Science Bulletin,2008,5(7):821-828.[况雪源,刘健,王红丽,等. 近千年来南北半球气候变化模拟比较[J]. 科学通报,2008,5(7):821-828.]
[44] Zheng Jingyun, Wang Shaowu. Assessment on climate change in China for the last 2000 years[J].Acta Geographic Sinica, 2005,60(1):21-31.[郑景云,王绍武,中国过去2000年气候变化的评估[J]. 地理学报,2005,60(1):21-31.]
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