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自从普莱斯托纪早期以来,前退对北方冰盖变化的持续影响
Stephen Barker1, Aidan Starr1, Jeroen van der Lubbe2
1School of Earth and Environmental Sciences, Cardiff University, Cardiff, UK.
概括
全球冰的体积变化主要是由100万年前的斜率驱动的. 在冰川周期期间,前进影响了冰盖的融化,特别是在普莱斯托纪中后期.
科学领域:
- 古气候学
- 四年纪地质学
- 气候变化
背景情况:
- 全球冰量变化在历史上与地球的轨道周期有关.
- 倾斜和偏移对冰河时代的相对影响,特别是在100万年前,仍然是研究的主题.
研究的目的:
- 在过去的170万年里, 调查斜率和前行在驱动冰川周期中的独特作用.
- 为了确定冰盖扩张和消融的时间和机制以应对轨道强迫.
主要方法:
- 分析了北大西洋170万年来的冰上浮游记录.
- 冰上漂流事件与地球轨道参数 (斜率和前行) 的相关性.
主要成果:
- 在斜率下降的过程中,冰盖的膨胀始终发生.
- 大规模的冰浪费 (剥离) 事件始终与前进的最小值有关.
- 在普莱斯托纪中期到晚期,前进驱动的消融和冰川终结之间的关联是显著的.
结论:
- 在100万年前,斜率是冰川周期的主要驱动因素.
- 大约100万年前北半球冰盖向南延伸后,前进在冰川终结中变得重要.
- 冰河时代的轨道强迫在整个四年纪呈现出不同的阶段.
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