概括
太阳紫外线辐射的变化与热带臭氧的变化相关. 这些发现表明,在11年的太阳周期中,上层平流层中臭氧发生了显著的转移,需要进一步测量紫外线辐射.
科学领域:
- 大气科学 大气科学
- 太阳物理 太阳物理
- 臭氧层研究 臭氧层研究
背景情况:
- 太阳紫外线 (UV) 辐射呈现周期性变化.
- 平流层中的臭氧度受到太阳活动的影响.
- 以前的模型表明,太阳循环和臭氧水平之间存在联系.
研究的目的:
- 研究太阳紫外线辐射变化与热带臭氧度之间的关系.
- 量化臭氧对太阳强迫反应的幅度.
- 在较长的太阳周期中推断上层平流层中潜在的臭氧变化.
主要方法:
- 1979年冬季太阳紫外线辐射数据的分析.
- 在同一时期,在热带地区测量区域平均臭氧值.
- 观察到的臭氧变化与理论计算的比较.
主要成果:
- 在太阳紫外线辐射中观察到13.5天的周期和1%的振幅变化.
- 热带臭氧值显示出0.25%至0.60%的相应变化.
- 观察到的臭氧反应与之前的计算一致,但可能略高估计.
结论:
- 太阳紫外线辐射的变化直接影响热带臭氧水平.
- 在48公里高度的臭氧可以在11年的太阳周期中经历高达12%的变化.
- 准确解释上层平流层臭氧变化需要测量接近200nm的太阳紫外线辐射.
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