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气候变化的天文理论 被引量:1

ASTRONOMICAL THEORY OF CLIMATIC CHANGES
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摘要 地球气候变化在 10~ 10 0ka (千年 )的时间尺度上表现出规则的周期性 ,它们主要受轨道日射变化控制 ,并能被很精确地计算到几百万年 .根据Milankovitch创立的天文理论 ,轨道变化是通过改变日射的季节分布和纬度分布来影响气候的 .黄赤夹角以 4 1ka的周期改变日射的纬度分布 ,而气候岁差以 19ka和 2 3ka的两个周期改变日射的季节分布 .作为对轨道日射变化的响应 ,全球气候在 10~ 10 0ka的时间尺度上按照气候岁差和黄赤夹角的周期变化 ,这一点已经为全新世气候的地质记录所验证 .轨道日射变化已经被证明是全新世冰期交替的重要原因 ,而且它仍然是现在和将来气候长期变化的重要原因 .因此 ,研究气候变化天文理论的重要性不仅仅在于了解过去年代的气候变化 ,也是为了更好地理解现在和将来的气候变化 .本文将简要介绍这个理论和相关的进展 . The earth's climatic changes show regular periodicities on the time scale of 10~100 ka, which are controlled by orbitally modulated variations in insolation and which can be calculated with great precision for several Ma. According to the astronomical theory of climatic changes that Milankovitch founded, the variations in the earth's orbit influence climate by changing the seasonal and latitudinal distribution of insolation. The obliquity of the ecliptic mainly controls the latitudinal distribution of insolation with a period of 41 ka. The climatic precession mainly controls seasonal distribution of insolation with two periods of 19 ka and 23 ka. In response to orbitally modulated variations in insolation, the global climate changes on the time scale of 10~100 ka with the periods of the precession and obliquity, which has been tested and verified by the geologic records in Pleistocene climate. Orbitally modulated variations in insolation have been shown to be the fundamental cause of the succession of Pleistocene ice age and continue to be the fundamental cause of the long term variations in the present and future climate. Therefore the importance of studying the astronomical theory of climatic changes is not only to learn the climatic changes in the past age but also to understand better the climatic changes in the present and future time. This paper presents a brief outline of the theory and relevant progress.
作者 苏旸
出处 《地球物理学进展》 CSCD 2000年第3期102-111,共10页 Progress in Geophysics
基金 国家自然科学基金项目!(199730 11 198330 30 )
关键词 气候变化 地球轨道 古气候学 日射变化 天文理论 Climatic changes Earth orbit insolation palaeoclimatology
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  • 1[1] Milankovitch M, Konigl erb. Akad. Beograd. Spec.1941, 132.
  • 2[2] Herbert D H, Fischer A G. Milankovitch climatic orgin of mid-Cretaceous black shale rhythms in central Italy. Nature, 1986,321: 739~743.
  • 3[3] Berger A, Louter M P, Tricot C. Insolation and Earth's orbital periods. J. Geophys. Res., 1993, 98: 10341~10362.
  • 4[4] Hays J D, Imbrie J, Shackleton N J. Variations in the Earth's Orbit: Pacemarker of the Ice Ages. Science, 1976, 194: 1121~1132.
  • 5[5] Imbrie J, Hays J D, Martinson D G, et al. The orbital theory of pleistocene climate: support from a revised chronologyof the marine δ18O record. In:Milankovich and Climate (Part 1), eds: Berger A, Imbrie J, Hays J D, et al. D.Reserdel Publ. Comp.(Holland), 1986, 269~305.
  • 6[6] Kukla G, Berger A, Lotti R, et al. Orbital signature of interglacials. Nature,1981,290:295~300.
  • 7[7] Vimeux F, Masson V, Jouzel J. Glacial-interglacial changes in ocean surface conditions in the Southem Hemisphere. Nature, 1999, 398: 410~413.
  • 8[8] Willis K J, Kleczkowski A, Crowhurst S J. 124,000-year periodicity in terrestrial vegetation change the late pliocene epoch. Nature, 1999, 397:685~688.
  • 9[9] Oerlemans J. Model experiments on the 100,000-year glacial cycle. Nature, 1980, 287: 430~432.
  • 10[10] Imbrie J, Imbrie J Z. Modeling the climatic Response to Orbital Variations. Science, 1980, 207:943~953.

同被引文献33

  • 1李平,彭子成,文启彬,李玉成,杨辉,洪阿实,许志峰,王明亮,业渝光,和杰,刁少波.福建宁化天鹅洞石笋年代和古温度[J].沉积学报,1996,14(1):149-155. 被引量:15
  • 2吕厚远,郭正堂,吴乃琴.黄土高原和南海陆架古季风演变的生物记录与Heinrich事件[J].第四纪研究,1996,16(1):11-20. 被引量:33
  • 3郭正堂,刘东生,吴乃琴,吕厚远,韩家.最后两个冰期黄土中记录的Heinrich型气候节拍[J].第四纪研究,1996,16(1):21-30. 被引量:91
  • 4郑淑蕙 侯发高 等.我国大气降水的氢氧同位素研究[J].科学通报,1983,13:801-806.
  • 5汪训一.桂林茅茅头大岩洞穴沉积物的放射性年龄及氧、碳同位素特征[J].科学通报,1985,30(7):528-531.
  • 6刘东生.桂林地区大气降水的氢氧同位素研究[J].中国岩溶,1987,6(3):12-15.
  • 7Imbriet J, Hays J D, Martinson D G, et al. The orbital theory of Pleistocene climate: support from a revised chronology of the marine d 18O record. In: Berger A, Imbrie J, Hays J D, et al, eds. Milankovich and Climaye. Part 1, Norwell MA: Reidel Press, 1984. 269~305
  • 8Martinson D G, Pisias N J, Hays J D, et al. Age dating and the orbital theory of ice ages: development of a high-resolution 1 to 300000 years chronostratigraphy. Quaternary Research, 1987, 27(1): 1~29
  • 9Shackleton N J, Opdyke N D. Oxygen isotope and palaeomagnetic stratigraphy of Pacific core V28-239 late Pliocene to latest Pleistocene. Geol Soc Am Memoir, 1976, 145: 449~464
  • 10Shackleton N J, Opdyke N D. Oxygen isotope and palaeomagnetic stratigraphy of equatorial pacific core V28-238: Oxygen isotope temperature and ice volumes on a 105 year and 10 6 year scale. Quaternary Research, 1973, 3: 39~55

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