概括
测量了北极地区的平流层臭氧 (O(3) 和二氧化 (NO(2) 水平,使用太阳光和月亮光进行测量. 在极旋中心附近观察到较低的O(3) 和NO(2) 值,表明动态过程和异质光化学.
科学领域:
- 大气化学 大气化学
- 石流层科学 石流层科学
- 北极地区环境监测
背景情况:
- 平流层臭氧 (O3) 和二氧化 (NO2) 是重要的大气成分.
- 了解它们在极地地区的变化对于气候研究至关重要.
- 北极极地影响大气的组成和化学成分.
研究的目的:
- 为了测量北极平流层中O ((3) 和NO ((2) 的总列丰度.
- 为了研究北极极地对这些气体丰度的影响.
- 评估北极冬季异质光化学的潜力.
主要方法:
- 用分散的阳光和直接的月光进行测量.
- 用两个波长范围进行光谱分析.
- 1988年1月29日至2月16日在格陵兰的图勒 (北极76.5度) 进行观测.
主要成果:
- 观察到的O(3) 列在325到400多布森单位之间变化.
- 较低的O(3) 值与北极极旋中心的距离相关.
- 二氧化的含量在中最低,达到5 x 10^14分子/厘米2,相当于南极春季的水平.
结论:
- 北极中的动态过程可能会降低O3水平.
- 在分析长期趋势时,必须考虑这些O(3) 变化.
- 低的NO2含量表明北极冬季发生了显著的异质光化学,类似于南极的条件.
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