气候变化 气候变化 由大气氧度造成的长期气候强迫
Christopher J Poulsen1, Clay Tabor2, Joseph D White3
1Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109, USA. poulsen@umich.edu.
概括
大气氧气水平的变化通过改变大气密度和短波辐射影响了地球的气候. 较高的氧气水平导致温度降低,而较低的氧气水平导致气候变暖.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 大气科学 大气科学
背景情况:
- 大气中的氧气 (O2) 含量在Phanerozoic Eon期间大幅波动 (10-35%).
- 这些O2变化主要与生物进化有关,以前没有被认为是气候变化的驱动因素.
研究的目的:
- 研究不同氧气 (pO2) 部分压力对地球气候动态的影响.
- 为了确定O2水平是否可以作为一个重要的气候强迫因素在整个地质时间.
主要方法:
- 用气候建模模拟来评估不同pO2水平的影响.
- 模拟分析了pO2如何影响大气质量,密度和光学深度.
主要成果:
- 在低pO2条件下的大气密度降低导致较少的短波散射,增加了表面短波强迫.
- 涉及潜在热量,海洋层云和水蒸气的反放大了变暖.
- 增加的pO2被证明可以增强温室强迫和全球表面温度.
结论:
- 氧的部分压力 (pO2) 被确定为在地质时间尺度上调节地球气候的关键因素.
- 氧气对大气密度和光学特性的影响直接影响气候强迫.
- 这项研究需要重新评估过去的气候动态,将O2水平作为关键变量纳入其中.
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