奥利戈纪气候系统的心跳
Heiko Pälike1, Richard D Norris, Jens O Herrle
1National Oceanography Centre, Southampton, School of Ocean and Earth Science, European Way, Southampton SO14 3ZH, UK. H.Palike@soton.ac.uk
概括
一个1300万年的气候记录揭示了一个全球碳循环"心跳",与轨道循环和冰河时代有关. 这表明地球的碳循环,太阳强迫和冰川事件之间存在着根本的相互作用.
科学领域:
- 古气候学 古气候学
- 地球系统科学 地球系统科学
- 海洋学 海洋学 海洋学
背景情况:
- 奥利古纪气候记录提供了对长期地球系统动态的见解.
- 已知轨道变化会影响地球的气候和冰河时代.
- 全球碳循环在调节气候方面发挥着至关重要的作用.
研究的目的:
- 研究轨道周期,全球碳循环和冰川事件之间的长期关系.
- 为了确定气候和碳循环动态的周期性在奥利古纪.
- 了解驱动气候系统对轨道强迫反应的机制.
主要方法:
- 从赤道太平洋的1300万年连续气候记录的分析.
- 识别冰川事件中的循环和碳循环.
- 盒子建模模,模拟碳循环和太阳强迫的相互作用.
主要成果:
- 一个发音的A.
- 心跳的心跳的心跳
- 在全球碳循环和冰川周期中被确定.
- 检测到的周期为405,000年,127,000年和96,000年的离心率,以及120万年的斜率.
- 40万5千年的异心周期被碳在海洋中的长期停留时间所放大.
结论:
- 气候系统展示了碳循环,太阳强迫和冰川事件之间的基本相互作用.
- 轨道变化调节深海酸度和全球生物质生产/埋葬.
- 海洋碳的长居留时间放大了长期的偏心周期.
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