地球科学进展 ›› 2005, Vol. 20 ›› Issue (9): 990 -998. doi: 10.11867/j.issn.1001-8166.2005.09.0990

干旱气象研究 上一篇    下一篇

全球气候变化及其影响因素研究进展综述
张强,韩永翔,宋连春   
  1. 中国气象局兰州干旱气象研究所,甘肃省干旱气候变化与减灾重点实验室,甘肃 兰州 730020
  • 收稿日期:2005-05-25 修回日期:2005-07-09 出版日期:2005-09-25
  • 通讯作者: 张强
  • 基金资助:

    国家科技部“西部开发科技行动”重大项目“祁连山空中云水资源开发利用研究”(编号:2004BA901A16);国家自然科学基金项目“利用现有观测资料确定西北干旱荒漠区陆面过程参数” (编号:40175004)资助.

THE SUMMARIZE OF DEVELOPMENT OF GLOBAL CLIMATE CHANGE AND ITS EFFECT FACTORS

ZHANG Qiang; HAN Yongxiang; SONG Lianchun   

  1. Lanzhou Institute of Arid Meteorology ,CMA,Lanzhou 730020, China
  • Received:2005-05-25 Revised:2005-07-09 Online:2005-09-25 Published:2005-09-25

概述了全球气候变化问题提出的科学背景,总结了引起气候变化的原因,客观分析了引起不同时间尺度气候变化的各种自然因素,透视了人类活动对气候变化的影响程度,讨论了应该如何理解当今全球气候变暖问题。同时,还综述了气候变化研究中的学术分歧和科学困惑。

In this paper, firstly, the science background is simply summarized about the global climate change,then based on the compartmentalized time scale,the cau global climate warming. change and its effect factors in different time scales are discussed. By analyzed the key natural factors which could cause the climate change in different time scales and the anthropogenic influence upon climate change,it will be help for us to understand the present global climate warming. At the same time,the science diverging and perplexity on the study of climate change are also reviewed.

中图分类号: 

[1] Zhang Lansheng,Fang Xiuqi,Ren Guoyu. Global Change[M]. Beijing:Higher Education Press,2001. 1-341.[张兰生,方修琦,任国玉. 全球变化[M]. 北京:高等教育出版社,2001.1-341.]
[2] Cheng Hai. The mutation study of global climate:Argue or act?[J]. Chinese Science Bulletin,2004,49(13):1 339-1 344.
[3] Schwartz P, Randall D. “Abrupt climate change,” report prepared by Global Business Network (GBN) for the Department of Defense[EB/OL]. http:www.gbn.org/ArticleDisplayServlet.srv?aid= 26231,2005.
[4] Lyell C. Principles of Geology, Being An Attempt to Explain the Former Changes of the Earth's Surface by Reference to Causes Now in Operation[M].London: John Murray,1830. 
[5] Agassiz L.  Tudes Sur Les Glaciers[M]. Neuch Tel:Privately Published, 1840.
[6] Savin S. The history of the Earth's surface temperature during the past 100 million years[J]. Annual Reviews of Earth and Planetary Science,1977,5:318-355.
[7] Savin S. Stable isotopes in climatic reconstructions[A]. In: Berger W H, Crowell J C ,eds.  Climate in Earth History[C]. Washington:National Academy Press, 1982. 164-171.
[8] Douglas R, Woodruff F. Deep sea benthic foraminifera[A]. In: Emiliani C ,ed. The Sea. Vol 7, The Oceanic Lithosphere[C]. New York: John Wiley, 1981.1 233-1 327.
[9] Moore T C, Pisias N G, Keigwin L D. Cenozoic variability of oxygen isotopes in benthic foraminifera[A]. In: Berger W H, Crowell J C,eds. Climate in Earth History[C]. Washington:National Academy Press, 1982.172-181.
[10] Miller K G, Fairbanks R G, Mountain G S. Tertiary oxygen isotope synthesis, sea level history, and continental margin erosion[J]. Paleoceanography,1987,2:1-19.
[11] Wolfe J A. Tertiary climates and floristic relationships at high latitudes in the Northern Hemisphere [J]. Palaeogeogr Palaeoclimatol Palaeoecol,1980,30:313-323.
[12] Wolfe J A, Poore R Z. Tertiary marine and non marine trends[A]. In: Berger W H, Crowell J C,eds.  Climate in Earth History[C]. Washington:National Academy Press, 1982.154-158.
[13] Wolfe J A. Climatic, floristic and vegetational changes near the Eocene Oligocene boundary in North America[A]. In: Prothero D R, Berggren W A,eds.  Eocene Oligocene Climate and Biotic Evolution[C]. Princeton:Princeton University Press,1992.421-436.
[14] Wolfe J A. Distribution of major vegetational types during the Tertiary[A]. In: Sundquist E T, Broecker W S,eds.  The Carbon Cycle and Atmospheric CO2: Natural Variations Archaean to Present[C].Washington: American Geophysical Union, 1985. 357-375.
[15] Heinrich H.  Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130 000 years[J]. Quaternary Research, 1988, 29: 142-152.
[16] Dansgaard W, Johnsen S J, Clausen H B, et al. Evidence for general instability of past climate from a 250 kyr ice core record[J]. Nature, 1993, 364: 218-220.
[17] Bond G, Broecker W, Johnsen S, et al.  Correlations between climate records from North Atlantic sediments and Greenland ice[J]. Nature, 1993, 365: 143 147.
[18] Broecker W S, Andree W, Wolfi H, et al. The chronology of the last deglaciation: Implication to the cause of the Younger Dryas event[J]. Paleoceanography, 1988, 3: 1 19.
[19] Pestiaux P, Mersch I V D, Berger A, et al. Paleocclimatic variability at frequencies ranging from 1 cycle per 10,000 years to 1 cycle per 1000 years: Evidence for nonlinear behavior of the Climate system[J]. Climate Change, 1988, 12: 9-13.
[20] Keigwin L D, Jones G A, Lehman S J, et al. Deglacial meltwater discharge, North Atlantic deep circulation and abrupt climate change[J]. Journal of Geophysical Research, 1991, 96(C6): 16 811-16 826.
[21] Hughen K A, Overpeck J T, Peterson L C, et al. Rapid climate changes in the tropical Atlantic region during the last deglaciation[J]. Nature, 1996, 380: 51-54.
[22] Peterson L C, Haug G H, Hughen K A, et al. Rapid changes in the hydrologic cycle of the Tropical Atlantic during the Last Glacial[J]. Science, 2000, 290: 1 947 1-951.
[23] Liu D S, Guo Z T. Geological environments in China and global change[A]. In: An Z S,ed. An Corpus of Liu Dongsheng[C].Beijing: Science Press, 1997.192-202.
[24] Porter S C, An Z S. Correlation between climate events in the North Atlantic and China during the last glaciation[J]. Nature, 1995,375: 305-308.
[25] Guo Z T, Liu T S, Fedoroff N, et al. Climate extremes in Loess of China coupled with the strength of deep water formation in the North Atlantic[J]. Global and Planetary Change, 1998, 18:113-128.
[26] Thompson L G, Yao T D, Davis M E, et al. Tropical cimate instability: The last glacial cycle from a Qinghai Tibetan ice core[J]. Science,1997, 276: 1 821-1 825.
[27] Thompson L G, Thompson M E, Sowers T A, et al. A 25000 year tropical climate history from Bolivian ice cores[J]. Science,1998, 282: 1 858-1 864.[28] Zachos J,Pagani M, Sloan L, et al. Trends, rhythms, and aberrations in global climate 65 Ma to present[J].Science,2001,292:686-699.
[29] Tang Maocang, Zhu Deqin, Gao Xiaoqing. Review and prospect of the research of Earth system's evolution[J]. Advances in Earth Science,2004,19(1):55 62. [ 汤懋苍,朱德琴,高晓清. 地球系统演化原因研究的回顾与展望[J].地球科学进展,2004,19(1):55-62.]
[30] Hay W W, Emanuel Soeding Robert M D,Christopher N W. The Late Cenozoic uplift climate change paradox [J]. International Journal of Earth Sciences,2002,91:746-774.
[31] Ruddiman W F, Prell W L. Introduction to the uplift climate connection[A]. In: Ruddiman W F,ed.  Tectonic Uplift and Climate Change[C]. New York:Plenum Press, 1997.3-15.
[32] Raymo M E, Ruddiman W F. Tectonic forcing of late Cenozoic climate[J]. Nature,1992,359:117-122.
[33] Li J J,Fang  X M. Uplift of Tibetan Plateau and environmental Changes[J]. Chinese Science Bulletin, 1999,44(23):2 117-2 124.
[34] Molnar P, England P.  Late Cenozoic uplift of mountain ranges and global climate change: Chicken or egg?[J].  Nature,1990,346:29-34.
[35] Ouyang Ziyuan,Wang Shijie,Xiao Zhifeng, et al. Palaeoenvironmental and palaeoclimate catastarophe induced by Cenozoic bolideimpact eventa [J].Quaternary Sciences,1995,(4):324-330.[欧阳自远,王世杰,肖志峰,等. 新生代地外物体撞击事件诱发的古气候环境灾变[J]. 第四纪研究,1995,(4):324-330.]
[36] France Lanord C, Derry L. Organic carbon burial forcing of the carbon cycle from Himalayan erosion[J]. Nature,1997,390:65-67.
[37] Quade J,Cerling T E,Brwman J R. Development of Asia monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan[J]. Nature,1989,342:162-166.
[38] Shi Yafeng,Li Jijun,Li Bingyuan. Late Cenozoic Uplift of Tibetan Plateau and Environmental Changes[M]. Guangzhou:Guangdong Science and Technology Press,1998.[施雅风,李吉均,李炳元. 青藏高原晚新生代隆升与环境变化[M]. 广州:广东科学技术出版社,1998.]
[39] Barron E J, Washington W M. The role of geographic variables in explaining paleoclimates: Results from Cretaceous climate model simulations[J]. Journal of Geophysical Research,1984,89:1 267- 1 279.
[40] Tang Maocang, Guo Weidong. The great ice age cycles associated with the variation of the atmospheric heat engine efficiency[J] . Science in China ( D),1998 ,28 (3) :284-288.[汤懋苍,郭维栋.大冰期成因的大气热机效率变化说[J].中国科学D辑,1998 ,28 (3) :284-288.]
[41] Schwarzacher W. The identification and analysis of stratification cycles[J]. Paleoceanography,1987,2:79-95.
[42] Muller R A, MacDonald G J.〖KG1〗Glacial cycles and astronomical forcing[J]. Science,1997,277:215-218.
[43] Chamberlin T C. An attempt to frame a working hypothesis of the cause of glacial periods on an atmospheric basis[J]. Journal of Geophysical Research,1899,7:545-787.
[44] Broecker W S. The end of the present interglacial: How and when?[J]. Quaternary Science Reviews,1998, 17: 689-694.
[45] Peter U C,Richard B A,David P. Northern hemisphere ice sheet influences on global climate change[J].Science,1999,286:1 104- 1 111.
[46] Peter U C,Shawn J M,Garry K C,et al.Freshwater forcing of abrupt climate change during the last glaciation[J].Science,2001,299:283-287.
[47] Pagani M, Arthur M A, Freeman K H. Miocene evolution of atmospheric carbon dioxide[J]. Paleoceanography,1999,14:273-292.
[48] Pagani M, Freeman K H, Arthur M A. Miocene atmospheric CO2- levels and the expansion of C4 grasses[J]. Science,1999,285:876-879.
[49] Pearson P N, Palmer M R. Declining atmospheric carbon dioxide in the last sixty million years[J]. Nature,2000,406:695 699.
[50] Veizer J, Godderis Y, Franξois L M. Evidence for decoupling of atmospheric CO2 and global climate during the Phanerozoic eon[J]. Nature,2000,408:698-701.
[51] EPICA Community Members. Eight glacial cycles from an Antarctic ice core[J].Nature,2004,429:623-628.
[52] Clement A C, Cane M A, Seager R. An orbitally driven tropical source for abrupt climate change[J]. Journal of Climate, 2001, 14:2 369-2 375.
[53] Stott L, Poulsen C, Lund S, et al. Super ENSO and global climate oscillations at millennial time scales[J]. Science, 2002, 297: 222-226.
[54] Visser K, Thunell R, Stott L. Magnitude and timing of temperature change in the indo Pacific warm pool during deglaciation[J]. Nature,2003, 421: 152-155.
[55] Friis C E,Lassen K. Length of the solar cycle: An indicator of solar activity closely associated with climate[J]. Science,1991,245:698.
[56] Xu Jinghua. Sun,climate and nation's great migration[J]. Science in China(D),1998,28(4):365-384.
[57] Tang Maocang, Liu Yanxiang,Guo Weidong. Climatic condition and Chinese history (1):SCL and Chinese climate[J]. Plateau Meteorlogy,2001,20(4):368-373.[汤懋苍,柳艳香,郭维栋. 天时、气候与中国历史上:黑子周长与中国气候[J]. 高原气象,2001,20(4):368-373.]
[58] Gao Xiaoqing, Tang Mancang, Zhu Deqin. Some thoughts on climate system and earth system [J]. Chinese Journal of Geophysical, 2004 ,47(2) :364-368. [高晓清,汤懋苍,朱德琴. 关于气候系统与地球系统的若干思考[J].地球物理学报,2004 ,47(2) :364-368.]
[59] Svensmark H. Cosmic rays and Earth’s climate[J]. Space Science Review,2000,93:155-166.
[60] Marsh N, Svensmark H. Cosmic rays, clouds, and climate[J]. Space Science Review,2000,94:375-380.
[61] Martin J H. Glacial interglacial CO2- change: The iron hypothesis[J]. Paleoceanography,1990,5:1-13.
[62] Boyd P W, Watson A J, Law C S, et al. A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization[J]. Nature,2000,407:695-702.
[63] Coale K H,Johnson K S, Stout P M, et al. A massive phytoplankton bloom induced by an ecosystem scale iron fertilization experiment in the equatorial Pacific Ocean[J]. Nature,1996,383:495-501.
[64] Abraham E R,Law C S, Boyd P W, et al. Importance of stirring in the development of an iron fertilized phytoplankton bloom[J]. Nature,2000,407:727-730. 
[65] Watson A J, Bakker D C E, Ridgwell A J, et al.  Effect of iron supply on Southern Ocean CO2- uptake and implications for glacial atmospheric CO2-[J]. Nature,2000,407:730-733.
[66] Ridgwell A J, Maslin M A,Watson A J. Reduced effectiveness of terrestrial carbon sequestration due to an antagonistic response of ocean productivity[J]. Geophysical Research Letter,2002,29,10.1029/2001GL014304.
[67] Zhuang Guoshun, Guo Jinghua, Yuan Hui, et al. Coupling and feedback between iron and sulphue in air sea exchange[J].Chinese Science Bulletin, 2003,48(11):1 080-1 086.
[68] Fang Xiaomin,Han Yongxiang,Ma Jinghui,et al. Dust storms and loess accumulation on the Tibetan Plateau: A case study of dust event on 4 March 2003 in Lhasa[J]. Chinese Science Bulletin, 2004,49(9): 953-960.
[69] Wu Guanjian, Yao Tandong, Thompson L G, et al. Microparticle record in the Guliya ice core and its comparison with polar records since the last interglacial[J]. Chinese Science Bulletin, 2004, 49(6): 607-611.
[70] Thomas J C. Causes of climate change over the past 1000 years[J]. Science,2000,289:270-277.
[71] Petit J R, Jouzel J, Raynaud, D, et al. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica [J]. Nature, 1999,399:429-436.

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[14] 林而达,王京华. 全球变化对农业的影响及适应对策[J]. 地球科学进展, 1995, 10(6): 597-604.
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