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大气中的二氧化碳和气候在过去的冰川时期的千年时间尺度上
1Department of Geosciences, Oregon State University, Corvallis, OR 97331-5506, USA. jinhoahn@gmail.com
概括
古代的二氧化碳 (CO2) 水平与南极温度相关,这表明南大洋对气候周期的影响. 二氧化碳的上升先于北半球变暖事件,为地球碳循环动态提供了洞察力.
科学领域:
- 古气候学 古气候学
- 地球系统科学 地球系统科学
- 气候动力学 气候动力学
背景情况:
- 了解过去的大气二氧化碳 (CO2) 变化对于破译全球碳循环和气候相互联系至关重要.
- 千年规模的气候动态为地球对温室气体变化的敏感性提供了洞察力.
研究的目的:
- 为了比较古代的二氧化碳变化与南极温度和北半球气候变化记录.
- 为了研究二氧化碳波动,南洋过程和突然气候变化之间的关系.
主要方法:
- 在千年时间尺度 (20,00090,000年前) 上分析二氧化碳变化.
- 与南极温度代理数据进行比较.
- 检查海洋沉积物代理和北大西洋深水 (NADW) 记录.
主要成果:
- 在千年级气候周期期间,在二氧化碳度和南极温度之间观察到正相关性.
- 快速的二氧化碳增加与北大西洋深水的积聚和南大洋分层的减少相吻合.
- 这些二氧化碳的增加发生在北半球寒冷时期 (阶段),而格陵兰的变暖事件之前.
结论:
- 南大洋的过程在千年时间尺度上对大气二氧化碳的调节起着重要作用.
- 海洋循环的变化,特别是NADW和南大洋分层,与二氧化碳的释放有关.
- 这些发现强调了海洋循环,二氧化碳水平和气候变化事件之间的复杂相互作用.
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