| 北半球臭氧总量与平流层环流关系的分析 |
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| 引用本文： | 郑光,吴统文.北半球臭氧总量与平流层环流关系的分析[J].高原气象,1991,10(3):277-286. |
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| 作者姓名： | 郑光 吴统文 |
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| 作者单位： | 中国科学院兰州高原大气物理研究所 甘肃省兰州市
(郑光，吴统文，贺慧霞)，中国科学院兰州高原大气物理研究所 甘肃省兰州市(瞿章) |
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| 基金项目： | 国家自然科学基金资助项目，兰州高原大气所青年科学基金资助项目 |
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| 摘 要： |
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| 关 键 词： | 臭氧 总量 平流层 环流 北半球 |
THE ANALYSIS OF THE RELATION BETWEEN TOTAL OZONE AND THE STRATOSPHERE CIRCULATION OVER THE NORTHERN HEMISPHERE |
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| Zheng Guang,Wu Tongwen,He Huixia Qu Zhang.THE ANALYSIS OF THE RELATION BETWEEN TOTAL OZONE AND THE STRATOSPHERE CIRCULATION OVER THE NORTHERN HEMISPHERE[J].Plateau Meteorology,1991,10(3):277-286. |
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| Authors: | Zheng Guang Wu Tongwen He Huixia Qu Zhang |
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| Abstract: | This paper consists of two parts, i. e. the annual variations of the total ozone and the stratospheric sudden warming (SSW) in Feb. 1981. The results show:
1. The total ozone and the stratosphere circulation are the same in seasonal variation. The polar vortex is corresponding with the high value of total ozone in winter; the polar high is corresponding with the low value in summer.
2. From winter to summer, the distribution of total ozone over the Northern Hemisphere and the lower stratospheric circulation are the same in transition time (May-June); from summer to winter, the former occurs in Oct.-Nov. , it is one month later than the latter(Sept.-Oct.).
3. The total ozone increases with increasing of the amplitude of the extra-long wave of the stratosphere during the whole year.
4. The total ozone distribution of the pre-stage(before two months) of the SSW is quite different from the secular mean distribution in that month.
5. The strength of the centre of the total ozone continuously increases more than 20% each month in the SSW place from the before two months of the SSW to the warming-month.
6. The total ozone maintains more than 10% of minus anomaly from the pre-stage to the post-stage (after two months) in the SSW place, i.e the SSW occurs in the place where the total ozone maintains minus anomaly for a long time. |
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| Keywords: | Total ozone Stratospheric circulation Annual variation Stratospheric sudden warming |
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