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Study on Ozone Change over the Tibetan Plateau
作者姓名:ZHOU Xiuji  LI Weiliang  CHEN Longxun  LIU Yu
作者单位:Chinese Academy of Meteorological Sciences Beijing 100081,Chinese Academy of Meteorological Sciences Beijing 100081,Chinese Academy of Meteorological Sciences Beijing 100081,Chinese Academy of Meteorological Sciences Beijing 100081
摘    要:This paper reviewed the main results with respect to the discovery of low center of total column ozone (TCO) over the Tibetan Plateau (TP) in summer, and its formation mechanism. Some important advances are summarized as follows: The fact is discovered that there is a TCO low center over the TP in summer, and the features of the background circulation over the TP are analyzed; it is confirmed that the TP is a pathway of mass exchange between the troposphere and stratosphere, and it influences the TCO low center over the TP in summer; models reproduce the TCO low center over the TP in summer, and the formation mechanism is explored; in addition, the analyses and diagnoses of the observation data indicate that not only there is the TCO low center over the TP in summer, but also TCO decrease trend over the TP is one of the strong centers of TCO decrease trend in the same latitude; finally, the model predicts the future TCO change over the TP.

关 键 词:青藏高原  臭氧  气候变化  大气圈  生态环境
收稿时间:5/9/2006 12:00:00 AM

Study on Ozone Change over the Tibetan Plateau
ZHOU Xiuji,LI Weiliang,CHEN Longxun,LIU Yu.Study on Ozone Change over the Tibetan Plateau[J].Acta Meteorologica Sinica,2006,20(2):129-143.
Authors:ZHOU Xiuji  LI Weiliang  CHEN Longxun  LIU Yu
Institution:Chinese Academy of Meteorological Sciences, Beijing 100081
Abstract:This paper reviewed the main results with respect to the discovery of low center of total column ozone (TCO) over the Tibetan Plateau (TP) in summer, and its formation mechanism. Some important advances are summarized as follows: The fact is discovered that there is a TCO low center over the TP in summer, and the features of the background circulation over the TP are analyzed; it is confirmed that the TP is a pathway of mass exchange between the troposphere and stratosphere, and it influences the TCO low center over the TP in summer; models reproduce the TCO low center over the TP in summer, and the formation mechanism is explored; in addition, the analyses and diagnoses of the observation data indicate that not only there is the TCO low center over the TP in summer, but also TCO decrease trend over the TP is one of the strong centers of TCO decrease trend in the same latitude; finally, the model predicts the future TCO change over the TP.
Keywords:the Tibetan Plateau (TP)  the TP ozone valley  pathway  total column ozone (TCO) decrease trend
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