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Volume 14 Issue 4

Oct.  1997

Article Contents
Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 1997 >  14(4): 505-512

Vertical Ozone Profile over Tibet Using Sage I and II Data

  • 1.

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


doi: 10.1007/s00376-997-0068-z

  • This paper discusses the vertical ozone distribution over Tibet using SAGE I and SAGE II data. The annual and seasonal vertical ozone profiles in 10.5-50.5 km a.s.l. over Tibet are analyzed to understand the vertical structure of low ozone value in this region, Regarding to the local ozone deficit, these profiles are compared with the vertical ozone distribution in the non-mountain areas at the same latitudes. The summer low ozone and the May maximum ozone deficit are detected from the SAGE data. The largest ozone deficit in May is found in 15.5-20.5 km a.s.l. centered at 16.5 km over this region. This ozone deficit can be related to the upward mass transfer described by poten-tial temperature variation over Tibet.
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    [2] Zou Han, Ji Chongping, Zhou Libo, Wang Wei, Jian Yongxiao, 2001: ENSO Signal in Total Ozone over Tibet, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 231-238.  doi: 10.1007/s00376-001-0016-2
    [3] Bo LIU, Juan HUO, Daren LYU, Xin WANG, 2021: Assessment of FY-4A and Himawari-8 Cloud Top Height Retrieval through Comparison with Ground-Based Millimeter Radar at Sites in Tibet and Beijing, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1334-1350.  doi: 10.1007/s00376-021-0337-2
    [4] Daren LU, Weilin PAN, Yinan WANG, 2018: Atmospheric Profiling Synthetic Observation System in Tibet, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 264-267.  doi: 10.1007/s00376-017-7251-7
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    [6] Jingmei Yang, Jinhuan Qiu, 2009: An Empirical Model for Estimating Stratospheric Ozone Vertical Distributions over China, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 352-358.  doi: 10.1007/s00376-009-0352-1
    [7] GAO Zhiqiu, BIAN Lingen, WANG Jinxing, LU Longhua, 2003: Discussion on Calculation Methods of Sensible Heat Flux during GAME/Tibet in 1998, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 357-368.  doi: 10.1007/BF02690794
    [8] Jiali MA, Xiuping YAO, 2023: Summer Extreme Precipitation in the Key Region of the Sichuan-Tibet Railway, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 843-855.  doi: 10.1007/s00376-022-2133-z
    [9] Liu Qijun, Zheng Xiangdong, Luo Chao, Ding Guoan, Li Xingsheng, Zhou Xiuji, 1997: Ozone Vertical Profile Characteristics over Qinghai Plateau Measured by Electrochemical Concentration Cell Ozonesondes, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 481-490.  doi: 10.1007/s00376-997-0066-1
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    [12] ZHOU Libo, ZOU Han, MA Shupo, LI Peng, ZHU Jinhuan, HUO Cuiping, 2011: Vertical Air Mass Exchange Driven by the Local Circulation on the Northern Slope of Mount Everest, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 217-222.  doi: 10.1007/s00376-010-9231-z
    [13] Sophie GODIN-BEEKMANN, Irina PETROPAVLOSKIKH, Stefan REIS, Paul NEWMAN, Wolfgang STEINBRECHT, Markus REX, Michelle L. SANTEE, Richard S. ECKMAN, Xiangdong ZHENG, Matthew B. TULLY, David S. STEVENSON, Paul YOUNG, John PYLE, Mark WEBER, Johanna TAMMINEN, Gina MILLS, Alkis F. BAIS, Clare HEAVISIDE, Christos ZEREFOS, 2017: The Quadrennial Ozone Symposium 2016, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 283-288.  doi: 10.1007/s00376-016-6309-2
    [14] Sophie GODIN-BEEKMANN, Irina PETROPAVLOSKIKH, Stefan REIS, Paul NEWMAN, Wolfgang STEINBRECHT, Markus REX, Michelle L. SANTEE, Richard S. ECKMAN, Xiangdong ZHENG, Matthew B. TULLY, David S. STEVENSON, Paul YOUNG, John PYLE, Mark WEBER, Johanna TAMMINEN, Gina MILLS, Alkiviadis F. BAIS, Clare HEAVISIDE, Christos ZEREFOS, 2018: Erratum to: The Quadrennial Ozone Symposium 2016, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 368-369.  doi: 10.1007/s00376-018-0001-7
    [15] Zhou Libo, Zou Han, Ji Chongping, Wang Wei, Jian Yongxiao, 2001: The Scandinavia Ozone Loss and Surface Heating, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 454-466.  doi: 10.1007/BF02919324
    [16] L.S. Hingane, 1989: Role of Ozone in the Sodium and Hydroxyl Nightglow, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 89-98.  doi: 10.1007/BF02656920
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    • Manuscript History

    Manuscript received: 10 October 1997
    Manuscript revised: 10 October 1997
    通讯作者: 陈斌, bchen63@163.com
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    Vertical Ozone Profile over Tibet Using Sage I and II Data

    • 1. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029
    • Manuscript received: 1997-10-10
    • Manuscript revised: 1997-10-10

    Abstract: This paper discusses the vertical ozone distribution over Tibet using SAGE I and SAGE II data. The annual and seasonal vertical ozone profiles in 10.5-50.5 km a.s.l. over Tibet are analyzed to understand the vertical structure of low ozone value in this region, Regarding to the local ozone deficit, these profiles are compared with the vertical ozone distribution in the non-mountain areas at the same latitudes. The summer low ozone and the May maximum ozone deficit are detected from the SAGE data. The largest ozone deficit in May is found in 15.5-20.5 km a.s.l. centered at 16.5 km over this region. This ozone deficit can be related to the upward mass transfer described by poten-tial temperature variation over Tibet.

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