干旱气候变化与可持续发展

全球大气臭氧层的主要特征和变化趋势

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  • 中国科学院大气物理研究所  北京  100029
曲绍厚

收稿日期: 1994-01-22

  网络出版日期: 1994-09-01

MAIN CHARACTERISTICS AND TRENDS IN GLOBAL OZONE LAYER

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  • Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029

Received date: 1994-01-22

  Online published: 1994-09-01

摘要

根据全球臭氧地面站(Dobson站、Brewer站、M83和M124站)总量资料、臭氧探空廓线资料和雨云卫星(TOMS、SAGE I 和 SAGE Ⅱ)臭氧总量和廓线资料,给出南、北半球特别是南极地区平流层臭氧主要特征和变化趋势。结果表明,无论是中、低纬地区还是高纬地区(特别是南极地区的“臭氧洞”)臭氧总工从70年代开始呈下降趋势,特别是近十几年来有加剧下降之势,这是各国政府和科学家极为关注的环境和气候问题。此外,还对臭氧总量变化趋势的各种解释作了综述。

本文引用格式

曲绍厚 . 全球大气臭氧层的主要特征和变化趋势[J]. 地球科学进展, 1994 , 9(5) : 39 -47 . DOI: 10.11867/j.issn.1001-8166.1994.05.0039

Abstract

On the basis of the total ozone and the ozone profile from global ground stations and satellite data (TOMS, SAGE I and SAGE B), this paper gives main characteristics and trends in the stratospheric ozone over the Northern Hemisphere and the Southern Hemisphere especially the Antarctica. The results show that from the 1970's the trends of the total ozone were decreased either over mid-latitude and low-latitude areas or over high-latitude areas, especially in the 10 odd years it has been an apparent downward trend. This trends have caused much attention from the scientists and politicians throughout the world. Besides, in the paper some interpretations on the trend or the total ozone are reviewed.

参考文献

[1] Stolarski R,Bojkov R, Bishop L, Zerefos C, Staehelin J and Zawodny J. Measuredtrendsin stratospheric ozone. Science,1992,256(5055):342-349.
[2] Farman J C, Gardiner B G and Shanklin J D. Large losses of total ozone in Antarctica reveal seasonal CIOx/Nox interaction. Nature,1985,315:207-210.
[3] Fels S B, Mahlman J D, Schwarzkopi M D and Sinclair R W. Stratospheric sensitivity to perturb alien in ozone and carbon dioxide:radiative and dynamical response. J Atmos Sci,1980,37:2265-2297.
[4] Whitten R C and Prasad S S. Ozone in free atmosphere. Van Nostrand Reinhold Company, New York ,1985.
[5] Atmospheric Environment Service, Canada. Ozone Data for the World,1991,No. 24.
[6] Gotz F W P, Gerlands Beitr. Geophys,1931,31:119.
[7] Scientific Assessment of Stratospheric Ozone 1989 and Monitoring Project, Report No.20, World Meteorlogical Organization, Geneva, Switzerland, 1990.
[8] Komhyr W D. NOAA Tech Mem ERL ARL-149 (NOAA/GMCC,Boulder,CO.),1986.
[9] Staehelin J and Schmidt W. Atmos Environ, 1991, 25A:1739.
[10] McCormick M P, Zawodny J M, Veiga R E, Larsen J C, Wang P H. An overview of SAGE I and II ozone measurements. Planet and Space Sci,1989,37:1567-1586.
[11] McCormick M P, Veiga R E, Chu W P. Stratospheric ozone profile and total ozone trends derived from the SAGE I and SAGE II data, Geophys Res Lett, 1992,19:269-272.
[12] Stolarski R S, Bloomfield P, McPeters R D and Herman J R. Totol ozone trends deduced from Nimbus 7 TOMS data. Geophys Res Lett, 1991,18:1015-1018.
[13] Stolarski R S, Schoeberl M R, Newman P A, McPeters R D, Krueger A J. The 1989 Antarctic ozone hole as observed by TOMS. Geophys Res Lett,1990,17:1267.
[14] 曲绍厚.南极上空“臭氧洞”形成和演变的分析研究.高原气象,1992,11(1):83-89.
[15] Chapman S. A theory of upper atmospheric ozone. R Meteor Soc Mem, 1930, (3):103-125.
[16] 言穆弘等.太阳活动、大气臭氧和平流层温度相关分析研究.高原气象,1993,12(3):302-311.
[17] 王贵勤等编译.大气臭氧研究.北京:科学出版社, 1985.
[18] 魏鼎文.论南极O3层空洞的形成及其演变趋势的预测.中国科学,1990,B辑(5) :545-552.
[19] 王明星.大气化学.北京:气象出版社,1991.

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