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南极冰川导致了海洋循环的变化,在Eocene-Oligocene过渡时期
A Goldner1, N Herold2, M Huber3
11] Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, Indiana 47907, USA [2] American Geophysical Union, Washington DC 20009, USA.
Nature
|August 1, 2014
概括
全球冷却和南极冰盖的增长是由大气中二氧化碳 (CO2) 的下降驱动的,而不是海洋门户的开放. 然后,冰盖的膨胀显著改变了海洋循环模式.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 气候建模气候模型
背景情况:
- 世 - 奥利古纪过渡 (大约3400万年前) 见证了全球冷却和南极冰盖的增长.
- 存在两个假设:南极热隔离通过门口开放或大气CO2的下降.
- 以前的代理数据显示了海洋学变化,但原因仍在争论中.
研究的目的:
- 区分网关的开放和二氧化碳的减少,作为南极冰川的驱动力.
- 为了研究南极冰盖增长对海洋循环的影响.
- 了解冰川和海洋学变化之间的反机制.
主要方法:
- 利用一个合的海洋-大气模型.
- 模拟的门户开放和南极冰盖增长的场景.
- 分析了海洋热分层和循环模式的变化.
主要成果:
- 南极冰盖的增长,而不是门口的开放,最好的解释是观察到的海洋学变化.
- 冰盖的扩张增强了南极洲中间水的向北运输.
- 刺激南极底层水的形成从根本上重组了海洋循环.
结论:
- 二氧化碳的吸收,而不是门口的开放,导致南极冰盖的增长.
- 南极冰川显著改变了海洋循环和热流.
- 这些动态,涉及复杂的反,可能会继续影响未来的气候.
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