最近北半球平流层HCl由于大气循环变化而增加
E Mahieu1, M P Chipperfield2, J Notholt3
1Institute of Astrophysics and Geophysics, University of Liège, Liège 4000, Belgium.
Nature
|November 7, 2014
概括
与预期相反,由于大气循环减慢,平流层水平正在增加. 这种趋势异常影响了臭氧层研究,需要考虑大气动态.
科学领域:
- 大气化学 大气化学
- 石流层科学 石流层科学
- 气候动力学 气候动力学
背景情况:
- 含气体,如化碳,从20世纪70年代到90年代,大气中的含量显著增加.
- 这些气体有助于臭氧层的损耗,导致蒙特利尔议定书和随后的表面的减少.
- 平流层在1996年后达到峰值,预计将下降,反映表面趋势.
研究的目的:
- 为了调查平流层化 (HCl) 最近意外增加的情况.
- 为了了解这种异常背后的驱动因素,与表面源气体的减少形成鲜明对比.
- 评估这一趋势对平流层臭氧层演变的影响.
主要方法:
- 对化 (HCl) 度的地面和卫星数据的分析.
- 使用大气模型模拟来解释观察到的趋势.
- 将平流层HCl趋势与源气体近地度进行比较.
主要成果:
- 从2007年左右开始,在北半球观察到平流层化 (HCl) 的显著增加.
- 这一趋势与近地表源气体持续减少形成鲜明对比.
- 模型模拟将异常归因于北半球大气循环放缓.
结论:
- 北半球大气循环的减缓导致平流层中酸盐的增加.
- 这种动态变化导致更老化的空气和更大的源气体转化为低层平流层中的化物.
- 未来对臭氧层的研究必须考虑这种短期的动态变化及其对平流层标记物的影响.
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