青藏高原冰芯研究进展

doi:10.11867/j.issn.1001-8166.1999.02.0183

地球科学进展 ›› 1999, Vol. 14 ›› Issue (2): 183 -188. doi: 10.11867/j.issn.1001-8166.1999.02.0183

所属专题：青藏高原研究——青藏科考虚拟专刊；

青藏高原冰芯研究进展

杨保 ^①,施雅风 ^①②

①中国科学院南京地理与湖泊研究所,江苏南京 210008；②中国科学院兰州冰川冻土研究所,甘肃兰州 730000

收稿日期:1998-05-25 修回日期:1998-08-18 出版日期:1999-04-01
通讯作者: 杨保,男,1971年5月生,博士生,主要研究方向为古气候的重建。
基金资助:
国家科委、中国科学院重大项目“亚洲地区气候变迁与全球变化”(项目编号:KZ951-A1-202-04)资助。

RESEARCH ADAVNCES OF ICE CORE RECORDS IN QINGHAI-TIBET PLATEAU

YANG bao ^①,SHI Yafeng ^②

①NanjingInstitute ofGeography andLimnology,Chinese Academy ofSciences,Nanjing 210008,China；②Lanzhou Institute ofGlaciology and Geocryology,Chinese Academy ofSciences,Lanzhou 730000,China

Received:1998-05-25 Revised:1998-08-18 Online:1999-04-01 Published:1999-04-01

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青藏高原冰芯研究是恢复该地区古气候、环境变化的有力手段,近年来取得了显著的成就。对青藏高原冰芯研究在稳定氧同位素、冰川积累量、冰芯的断代以及冰芯记录的环境指标等四个方面的研究进展进行了详细的评述,总结了冰芯记录所恢复的气候、环境变化研究成果,并对当前青藏高原冰芯研究中存在的问题和今后的发展趋势进行了探讨。

关键词: 青藏高原, 冰芯研究, 环境变化

As a robust tool of reconstructing palaeo-climate and palaeo-enviroment,study on ice cores ofQinghai-Tibet Plateau has obtained striking achievements in recentyears.This paper has in detail analyzed and discussed stable oxygen isotope,glacial accumulation,the dating technique of ice core and environmental indices recorded in ice core.Based on the discussions above,the research results of climatic and environmental changes restored by the ice ore records has been summarized,such as reconstructed climatic and environmental series at different time scale(including the Little Ice Age,millennial scale,1 000-year-scale series),consistences and similarities in climatic change between ice core records and other areas aswell as the discoveryof climatewarming in the 20th century.In addition,current problems and developmental tendencies of ice core study in Qinghai-Tibet Plateau have been suggested.As stated below:(1)More robust functional relationship between stable oxygen isotope and temperature will be perfected;(2)Comparison and analysis of ice core records in Qinghai-Tibet Plateau with those of its surrounding areas and even North Hemisphere at different time scale and defferent resolution are playing an important role in studying climatic variations.(3)Contents and scope on ice core research on Qinghai-Tibet Plateau are to develop and extend.(4)Determination of greenhouse gases and rare gases closed in ice core bubbles tend to be an important aspect in ice core study.(5)Research on stage,abrupt change and mechanism of climatic and environmental evolution will be strengthened.

Key words: Qinghai-Tibet plateau, Ice core study, Environmental change.

中图分类号:

P343·
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〔1〕姚檀栋.青藏高原海拔7 000米冰芯的钻取及其意义.冰川冻土,1998,20(1):1~2.
〔2〕姚檀栋,丁良福,蒲建成,等.青藏高原唐古拉山地区降雪中δ18O特征及其与水汽来源的关系.科学通报,1991,(20):1 570~1 573.
〔3〕章新平,姚檀栋.我国部分地区降水中氧同位素成分与温度和降水量之间的关系.冰川冻土,1994,16(1):31~40.
〔4〕Yao Tandong,Thompson L G.Trends and features of climatic changes in the past 5 000 years records by the Dunde ice core.Ann Glaciol,1992,16:21~24.
〔5〕章新平,姚檀栋.影响青藏高原的天然系统与降水中氧同位素的关系.冰川冻土,1995,17(7):124~131.
〔6〕章新平,施雅风,姚檀栋.青藏高原东北部降水中δ18O的变化特征.中国科学(B辑),1995,25(5):540~547.
〔7〕章新平,姚檀栋.青藏高原降水中δ18O与温度和降水量的关系.地理科学,1995,15(1):1~7.
〔8〕Yao Tandong,Thompson L G,Jiao Keqin,et al.Recent warming as Recorded in the Qing-hai-Tibetan cryosphere.International of Glaciological Society.Cambridge uk,Annals of Glaciology,1995,21:196~200.
〔9〕Yao Tandong,Thompson L G,Mosley Thompson,et al.Climatological significance ofδ18O in north Tibetan ice core.Journal of Geophysical Research,1996,Vol.101(23):29 531~29 537.
〔10〕姚檀栋,Thompson LG.敦德冰芯记录与过去5 ka温度变化.中国科学(B辑),1992,(10):1 089~1 093.
〔11〕Thompson L G,et al.Holocene-late pleistocene climatic ice core records from Qinghai-Tibbetan Plateau.Science,1989,(246):474~477.
〔12〕谢自楚,武筱苓,姚檀栋,等.敦德冰岩芯古气候环境记录的初步研究,1989,(2):135~142.
〔13〕姚檀栋,谢自楚.敦德冰岩芯研究及其意义.中国西部第四纪冰川与环境.中国第四纪冰川与环境研究中心.中国第四纪研究委员会编,科学出版社,1996.24~32.
〔14〕Yao Tandong,Qin Dahe,TianLide,et al.Variations in temperature and precipitation in the past 2 000 a on the XiZang(Tibet) Plateau-Guliya ice core record(in Chinese).Science in China(Ser D),1996,26(4):348~353.
〔15〕姚檀栋,薄建辰,刘景寿.唐古拉冰芯气候学研究.见:青藏高原冰川气候与环境.北京:科学出版社,1993.16~21.
〔16〕姚檀栋,Thompson L G,施雅风,等.古里雅冰芯中末次间冰期以来气候变化记录研究.中国科学(D辑),1997,27(5):447~452.
〔17〕Thompson LG,YaoTangdong,DavisME,et al.Tropical Climate Instability:The Last Glacical Cycle from a Qinghai-Tibetan Ice Core.Science,1997,276(20):1 822~1 825.
〔18〕Thompson L G, Mosley Thompson,Davis ME,et al.Glacial stage ice core records from the subtropical Dunde ice cap,China.Ann Glaciology,1990,14:288~297.
〔19〕Thompson L G and 7 others.Climate since AD 1510 on Dyer Plateau,Antractica Peninsula:evidence for recent climate change.Ann Glaciology,1995,(20):420~426.
〔20〕姚檀栋,盛文坤,杨志红.青藏高原的冰雪化学研究,青藏高原冰川气候和环境.北京:科学出版社,1993.8~15.
〔21〕李月芳,姚檀栋,皇翠兰.古里雅冰帽中化学成分的空间变化.冰川冻土,1993,15(3):467~473.
〔22〕姚檀栋,施雅风,杨志红.中国西部冰芯中的小冰期气候记录.第五届全国冰川冻土学大会论文集(上册).兰州:甘肃文化出版社,1996.99~106.
〔23〕施雅风,姚檀栋,杨保.近2000年古里雅冰芯年代际气候变化及其与中国东部文献记录的比较.待版.
〔24〕姚檀栋,焦克勤,李忠勤,等.古里雅冰帽气候环境记录.中国科学(B辑),1994,24(7):766~773.
〔25〕姚檀栋,焦克勤,杨志红,等.古里雅冰芯中小冰期以来的气候变化.中国科学(B辑),1995,25(10):1 108~1 114.
〔26〕姚檀栋,秦大河,田立德,等.青藏高原2 ka来温度和降水变化—古里雅冰芯记录.中国科学(D辑),1996,26(4):348~353.
〔27〕姚檀栋,焦克勤,皇翠兰,等.冰芯所记录的环境变化与空间耦合特征.第四纪研究,1995,(1):32.
〔28〕Thompson L G, Mosley Thompson, Davis M E,et al. A 1 000 year climate ice-core record fromthe Guliya ice cap, China: ita relationship to global climate variability. Ann Glaciology,1995,(21):175~181.
〔29〕Lin P N,Thompson L G,Davis M E,et al.1 000 years of climatic change in China: ice-Coreδ18O evidence.Ann Glaciology,1995,(21):189~195.
〔30〕Thompson L G.Ice core evidence from Peru and China.In:Bradley,RS and Jones,eds.Climate Since AD 1500.Routledge,London,1992.517~548.
〔31〕Yao Tandong,Jiao Keqin,Tian Lide,et al. Clmatic variations since the Little Ice Age Recorded in the Guliya ice core.Science in China,1996,39:587~596.
〔32〕姚檀栋,杨志红,刘景奉.冰芯记录所揭示的青藏高原升温.科学通报,1994,39(5):438~441.
〔33〕施雅风.冰芯记录揭示的气候变化.见:丁一汇等编.中国的气候变化与气候影响研究.北京:气象出版社,1997.6~17.
〔34〕HughesMK,Diaz H F.Was there a“Medieval Warm Period”,and if so,where and if so,where and when? Climatic Change,1994,(25):109~142.

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