关于"大气氧度的长期气候强迫"的评论
1School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia, Canada.
概括
低大气氧气可能不会像之前所说的那样温暖气候. 辐射和大气压力变化可能会导致冷却,这与之前的发现相矛盾,需要对气候模型进行进一步的研究.
科学领域:
- 地球科学
- 古气候学
- 大气科学
背景情况:
- 波尔森和其他人 提出了减少法内罗纪大气中的氧气水平会导致气候变暖.
- 这种假设与已确定的原理相反,其中较低的压力和改变的辐射转移通常会诱导冷却.
研究的目的:
- 重新评估大气中氧气水平与法内罗纪时期全球气候之间的关系.
- 调查拟议的变暖和预期的冷却效应之间的差异.
主要方法:
- 在气候模型中分析辐射转移过程.
- 在不同压力条件下检查大气结构的变化.
- 对模型输出进行比较以确定不一致.
主要成果:
- 与氧气减少相关的较低大气压会导致冷却效应.
- 低压下的辐射转移变化也会导致气候变冷.
- 现有的气候模型在氧气水平和温度方面呈现出相互矛盾的结果.
结论:
- 声称较低的世氧气水平导致了变暖需要进一步审查.
- 需要对观察到的模型冲突进行详细的机制解释.
- 进一步的研究应该集中在气候模型中的辐射和云过程的表现上.
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