大气中二氧化碳度的变化是早期代农纪气候的主要驱动因素
Eleni Anagnostou1, Eleanor H John2, Kirsty M Edgar2,3
1Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK.
Nature
|April 26, 2016
概括
早期欧气候最佳时期是6500万年来最温暖的时期. 新的研究表明,二氧化碳 (CO2) 含量约为1,400 ppm,导致了这种升温和随后的降温.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
背景情况:
- 早期纪气候最佳时期 (Early Eocene Climate Optimum,EECO) 是过去6500万年来最温暖的时期,温度比工业化前水平高出10°C以上.
- 随之而来的地球冷却是在伊纪,导致南极冰盖的形成.
- 以前对大气中二氧化碳 (CO2) 水平 (5003,000 ppm) 的估计缺乏精度,阻碍了对碳气候相互作用的理解.
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