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Long-term changes in total ozone column content and its association with stratospheric temperature over two neighbouring tropical Asian stations

机译:两个相邻热带亚洲站臭氧总含量的长期变化及其与平流层温度的关系

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摘要

This paper focuses on the long-term declining change in total ozone column (TOC) derived from satellite measurements over a 25 year period over two neighbouring tropical Asian sites, Karachi, and Mt Abu. A strong declining trend was observed in TOC at both sites, with a significance level of over 95% and a higher magnitude of 4 to 10 DU per decade in September to December and a weak statistical significance level of below 85% and a lower magnitude of 2 to 4 DU per decade in pre-monsoon months. However, during the monsoon months, a small declining trend of about 1 DU per decade was observed, but this variation is statistically insignificant. Further, the long-term changes in TOC exhibit seasonal dependence with a more negative change of 10 DU per decade in winter over Karachi and 7 DU per decade over Mt Abu. The consequence of such a net long-term declining change in TOC as high as 10 DU per decade is expected to have serious environmental implications due to an overall increase in ground-level solar UV radiation of 18% over the normal values in the tropics. In order to identify some plausible causes of this depletion trend in ozone concentration with stratospheric temperature and solar activity, it is clear that there is a strong relationship between the seasonal dependence of the long-term declining trend of TOC on air temperature at 10 mb or stratospheric cooling. At the same time, there is a less significant long-term variation in TOC due to altered solar activity levels.
机译:本文着重于在25年内对两个相邻的亚洲热带站点卡拉奇和阿布山的卫星测量得出的总臭氧柱(TOC)的长期下降趋势。在两个地点的总有机碳中均观察到了强烈的下降趋势,其显着性水平超过95%,9月至12月的十年间每10 DU的显着性较高,统计显着性水平低于85%的低显着性,而显着性水平较低。在季风前的几个月,每十年2至4 DU。但是,在季风月份中,观察到每十年约有1 DU的小幅下降趋势,但是这种变化在统计上是微不足道的。此外,TOC的长期变化表现出季节依赖性,在卡拉奇冬季每10年10 DU的负变化更大,在阿布山每10年7 DU的负变化更大。这样的TOC净长期长期下降变化的结果是每十年10 DU,这将对环境造成严重影响,这是因为地面太阳紫外线辐射的总体增加量比热带地区的正常值高18%。为了确定平流层温度和太阳活动导致臭氧浓度下降趋势的某些可能原因,很明显,TOC长期下降趋势对气温在10 mb或10 mb时的季节依赖性与季节之间存在很强的关系。平流层冷却。同时,由于太阳活动水平的变化,TOC的长期变化不太明显。

著录项

  • 来源
    《International journal of remote sensing》 |2013年第20期|6496-6506|共11页
  • 作者

    B.M. Vyas; Vimal Saraswat;

  • 作者单位

    Department of Physics, M. L. Sukhadia University, Udaipur 313 001, India;

    Department of Basic Sciences, Pacific College of Engineering, Udaipur 313 003, India;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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