在冰川和早期冰川间气候条件下突然释放到大气中
C Nehrbass-Ahles1,2,3, J Shin4, J Schmitt5,2
1Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland. cn425@cam.ac.uk.
概括
在寒冷和温暖的气候中都会出现二氧化碳的飞跃, 这些事件与海洋循环的变化以及热带降雨模式的变化有关.
科学领域:
- 古气候学
- 气候科学
- 地球系统科学
背景情况:
- 之前人们认为二氧化碳释放脉冲只发生在冰川时期.
- 人们认为温暖的气候条件缺乏这些突然的二氧化碳释放事件.
研究的目的:
- 研究二氧化碳跳跃 (CDJ) 在地球过去的气候中发生的情况,特别是在33万至45万年前.
- 要确定CDJ是否在寒冷和温暖的气候条件下发生.
主要方法:
- 分析高分辨率的二氧化碳记录,
- 二氧化碳波动与气候条件和海洋循环模式的相关性.
主要成果:
- 在寒冷和温暖的气候条件下都发现了明显的二氧化碳跳跃 (CDJ).
- 观察到两种类型的CDJ,与大西洋南部翻转循环 (AMOC) 和热带融合区的变化有关.
- 如果陆地冰通过淡水输入对AMOC产生重大影响,CDJ可能会在间冰期发生.
结论:
- 二氧化碳的跳跃是碳循环的普遍特征, 不仅限于冰川时期.
- 跨冰期CDJ可能发生在扩展的陆地冰块破坏AMOC时.
- 海洋循环动态在百年时间尺度上对大气二氧化碳的调节起着至关重要的作用.
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