概括
新的测量显示,平流层中氧基 (HO(2) 度与理论一致,高达40公里. 在这个高度以上,HO(2) 水平超过预测,可能是由于臭氧低估.
科学领域:
- 大气化学 大气化学
- 石流层科学 石流层科学
- 化学动力学 化学动力学
背景情况:
- 氧基 (HO2) 对于通过HOx催化循环破坏平流层臭氧至关重要.
- 以前对平流层HO(2) 的测量产生了相互矛盾的结果,其中一些超出了理论预测.
研究的目的:
- 为了准确测量平流层的氧基 (HO) (2) 概况.
- 将实验HO(2) 数据与理论模型进行比较.
主要方法:
- 使用气球载远红外光谱仪进行HO(2) 测量.
- 在白天和夜晚条件下进行了形测量.
主要成果:
- 白天HO(2) 档案与理论预测非常接近,高达40公里的高度.
- 在40公里以上,测量HO(2) 的混合比率大约比理论预测高出30%.
- 夜间HO(2) 档案明显低于白天档案,与理论预期一致.
结论:
- 这项研究提供了关于平流层HO2度的新的,可靠的数据.
- 40公里以上的差异表明目前大气模型中臭氧度的潜在低预测.
- 这些发现有助于更好地了解平流层中臭氧消耗机制.
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