极地海洋和冰川周期在大气中的CO2度
Daniel M Sigman1, Mathis P Hain, Gerald H Haug
1Department of Geosciences, Guyot Hall, Princeton University, Princeton, New Jersey 08544, USA. sigman@princeton.edu
Nature
|July 3, 2010
概括
在冰河时代,南大洋可能吸收了更多的二氧化碳 (CO2),减少了大气中的CO2. 这表明海洋二氧化碳的吸收是调节气候的关键.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 全球气候和大气中的二氧化碳 (CO2) 水平随着冰川时期的周期性波动而波动.
- 较低的大气二氧化碳度是冰河时代的特征,但潜在的机制仍然不清楚.
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