大气二氧化碳和南极温度变化的时间跨越终点III
Nicolas Caillon1, Jeffrey P Severinghaus, Jean Jouzel
1Institut Pierre Simon Laplace/Laboratoire des Sciences du Climat et de l'Environnement, Commissariat à l'Energie Atomique/CNRS, L'Orme des Merisiers, CEA Saclay, 91191, Gif sur Yvette, France. ncaillon@ucsd.edu
概括
温室气体变化在终结III期间将南极变暖延迟了800年,这表明温度和大气二氧化碳水平之间的复杂相互作用. 这一发现完善了我们对过去气候动态的理解.
科学领域:
- 古气候学 古气候学
- 冰芯分析 冰芯分析
- 气候变化研究 气候变化研究
背景情况:
- 冰芯分析提供了温室气体记录,但气体年龄与冰河年龄的差异造成了时间不确定性.
- 准确的过去气候事件的时间表对于理解气候动态至关重要.
研究的目的:
- 解决过去气候转型期间温室气体变化和温度波动之间的时间差异.
- 用沃斯托克冰芯数据调查终结III期间事件的顺序.
主要方法:
- 从沃斯托克冰芯的气泡中分析的同位素组成.
- 专注于终止III时期 (大约. 在24万年前).
主要成果:
- 同位素记录可能反映了终结III期间的温度和积累变化.
- 二氧化碳 (CO2) 的增加使南极的变暖延迟了800 +/- 200年.
- 二氧化碳的增加先于北半球脱冰.
结论:
- 这项研究改进了过去气候变化事件的时间表.
- 温室气体的增加跟随,而不是导致,最初的南极变暖.
- 这对理解气候反机制有影响.
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