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Volume 19 Issue 2

Mar.  2002

Article Contents
Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2002 >  19(2): 279-286

Variation Features of Total Atmospheric Ozone in Beijing and Kunming Based on Dobson and TOMS Data

  • 1.

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


doi: 10.1007/s00376-002-0022-z

  • About 20 years of Dobson and TOMS data are used to analyze the variation characteristics of total atmospheric ozone in Beijing (39.93°N, 116.40°E) and Kunming (25.02°N, 102.68°E). It is shown that:(1) the long-term change trends for 1979 (or 1980)-2000 period are -0.642 DU / year and -0.009 DU / year respectively in Beijing and Kunming, (2) there are strong intra-seasonal variations especially in wintertime.which are comparable to seasonal variations both in Beijing and Kunming, (3) the long-term trend deduced from shorter time period of record is significantly different from that for longer time period, both in Kunming and Beijing, (4) there are significant QBO signals both in Beijing (mid latitude) and Kunming (low latitude), (5) the inter-annual variations of atmospheric ozone in both stations are mainly composed of the long-term trend and QBO signals, and (6) our Dobson and TOMS measurements of total ozone are generally in good agreement.
  • [1] ZHANG Dingyuan, LIAO Hong, WANG Yuesi, 2014: Simulated Spatial Distribution and Seasonal Variation of Atmospheric Methane over China: Contributions from Key Sources, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 283-292.  doi: 10.1007/s00376-013-3018-y
    [2] Zou Han, Ji Chongping, Zhou Libo, 2000: QBO Signal in Total Ozone over Tibet, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 562-568.  doi: 10.1007/s00376-000-0019-4
    [3] LI Jiawei, HAN Zhiwei, 2012: A Modeling Study of Seasonal Variation of Atmospheric Aerosols over East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 101-117.  doi: 10.1007/s00376-011-0234-1
    [4] LI Wei, CHEN Longxun, 2003: Characteristics of the Seasonal Variation of the Surface Total Heating over the Tibetan Plateau and Its Surrounding Area in Summer 1998 and Its Relationship with the Convection over the Subtropical Area of the Western Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 343-348.  doi: 10.1007/BF02690792
    [5] LIU Xiangcui, LIU Hailong, 2014: Heat Budget of the South-Central Equatorial Pacific in CMIP3 Models, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 669-680.  doi: 10.1007/s00376-013-2299-5
    [6] Pucai WANG, N. F. ELANSKY, Yu. M. TIMOFEEV, Gengchen WANG, G. S. GOLITSYN, M. V. MAKAROVA, V. S. RAKITIN, Yu. SHTABKIN, A. I. SKOROKHOD, E. I. GRECHKO, E.V. FOKEEVA, A. N. SAFRONOV, Liang RAN, Ting WANG, 2018: Long-Term Trends of Carbon Monoxide Total Columnar Amount in Urban Areas and Background Regions: Ground- and Satellite-based Spectroscopic Measurements, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 785-795.  doi: 10.1007/s00376-017-6327-8
    [7] Hengyi WENG, 2003: Impact of the 11-yr Solar Activity on the QBO in the Climate System, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 303-309.  doi: 10.1007/s00376-003-0017-4
    [8] CHEN Wen, WEI Ke, 2009: Interannual Variability of the Winter Stratospheric Polar Vortex in the Northern Hemisphere and their Relations to QBO and ENSO, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 855-863.  doi: 10.1007/s00376-009-8168-6
    [9] Bo SUN, Huijun WANG, 2017: A Trend towards a Stable Warm and Windless State of the Surface Weather Conditions in Northern and Northeastern China during 1961-2014, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 713-726.  doi: 10.1007/s00376-017-6252-x
    [10] Zhang Ren, Yu Zhihao, 2000: Low-Frequency CISK-Rossby Wave and Stratospheric QBO in the Tropical Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 311-321.  doi: 10.1007/s00376-000-0012-y
    [11] Qian Yongfu, Zhang Qiong, Yao Yonghong, Zhang Xuehong, 2002: Seasonal Variation and Heat Preference of the South Asia High, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 821-836.  doi: 10.1007/s00376-002-0047-3
    [12] Xiuzhen LI, Wen ZHOU, Yongqin David CHEN, 2016: Detecting the Origins of Moisture over Southeast China: Seasonal Variation and Heavy Rainfall, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 319-329.  doi: 10.1007/s00376-015-4197-5
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    [16] Peng Yongqing, Yan Shaojin, 1994: Seasonal Variation Features of Western North Pacific Tropical Cyclone Tracks with Their Predictability, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 463-469.  doi: 10.1007/BF02658167
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    • Manuscript History

    Manuscript received: 10 March 2002
    Manuscript revised: 10 March 2002
    通讯作者: 陈斌, bchen63@163.com
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      沈阳化工大学材料科学与工程学院 沈阳 110142

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    Variation Features of Total Atmospheric Ozone in Beijing and Kunming Based on Dobson and TOMS Data

    • 1. LAGEO, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,LAGEO, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,LAGEO, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,LAGEO, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029
    • Manuscript received: 2002-03-10
    • Manuscript revised: 2002-03-10

    Abstract: About 20 years of Dobson and TOMS data are used to analyze the variation characteristics of total atmospheric ozone in Beijing (39.93°N, 116.40°E) and Kunming (25.02°N, 102.68°E). It is shown that:(1) the long-term change trends for 1979 (or 1980)-2000 period are -0.642 DU / year and -0.009 DU / year respectively in Beijing and Kunming, (2) there are strong intra-seasonal variations especially in wintertime.which are comparable to seasonal variations both in Beijing and Kunming, (3) the long-term trend deduced from shorter time period of record is significantly different from that for longer time period, both in Kunming and Beijing, (4) there are significant QBO signals both in Beijing (mid latitude) and Kunming (low latitude), (5) the inter-annual variations of atmospheric ozone in both stations are mainly composed of the long-term trend and QBO signals, and (6) our Dobson and TOMS measurements of total ozone are generally in good agreement.

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