冰芯记录了大气中的二氧化碳在最后三个冰川终点周围的记录
1Scripps Institution of Oceanography, Geosciences Research Division, University of California San Diego, La Jolla, CA 92093-0220, USA.
概括
古老的冰芯显示,在过去的变暖事件发生600年后,二氧化碳水平上升. 在冰河时代,二氧化碳的高度持续存在,这与之前的温暖时期和生物圈变化有关.
科学领域:
- 古气候学 古气候学
- 气候科学 气候科学
- 地球系统科学 地球系统科学
背景情况:
- 极地冰芯保存着古老的气泡,提供了关于过去大气组成的关键数据.
- 了解过去的温室气体动态对于预测未来的气候变化至关重要.
- 重建全球碳循环为地球气候敏感性提供了洞察力.
研究的目的:
- 分析过去气候变暖与大气二氧化碳 (CO2) 度之间的关系.
- 为了调查二氧化碳相对于脱冰事件的增加时间和持续时间.
- 探索陆地生物圈和冰盖动态在长期碳循环反中的作用.
主要方法:
- 来自南极冰芯的高分辨率记录的分析.
- 测量被困的气泡,以确定过去的二氧化碳度.
- 二氧化碳数据与来自冰核记录的古气候指标的相关性.
主要成果:
- 南极冰芯数据显示,二氧化碳度在过去三次脱冰开始后的600±400年增加了80100ppm.
- 在冰川时期观察到持续高的二氧化碳水平,即使温度下降.
- 前一个温暖时期的持续时间似乎影响了脱冰过程中的二氧化碳相位延迟.
结论:
- 在变暖事件和随后的二氧化碳增加之间存在显著的时间滞后,这表明复杂的反机制.
- 陆地生物圈和陆地冰覆盖的变化在冰川-冰川间周期中调节大气二氧化碳方面发挥着至关重要的作用.
- 过去的气候动态突出了地球系统中缓慢但强大的反,影响了长期的碳循环稳定性.
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