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开放系统的珊瑚年龄揭示了持续的次轨道海平面周期
William G Thompson1, Steven L Goldstein
1Lamont-Doherty Earth Observatory (LDEO) and Department of Earth and Environmental Sciences, Columbia University, Palisades, NY 10964, USA. wthompson@whoi.edu
概括
全球海平面的变化显示出频繁的振荡,这些振荡并不能由地球轨道变化解释. 一种新的约会方法改善了海平面的重建,揭示了这些持续的,快速的气候变化.
科学领域:
- 古气候学 古气候学
- 地质时间学 (Geochronology)
- 气候科学 气候科学
背景情况:
- 海平面是全球气候变化的关键指标.
- 众所周知,地球轨道的变化会在很长的时间范围内影响海平面 (至少有21000年的周期).
- 由于-珊瑚年代的局限性,对轨道以下频率的海平面变化进行准确的重建是具有挑战性的.
研究的目的:
- 开发一种更准确的方法来重建过去的海平面变化.
- 为了调查频繁的海平面振荡的原因.
- 为了更好地了解气候动态,解决轨道以下频率的海平面变化.
主要方法:
- 采用了一种新的方法来纠正珊瑚的年龄,以纠正系列核素的开放系统行为.
- 这种方法提高了海平面重建的精度和分辨率.
- /测年技术得到了改进,以克服以前的局限性.
主要成果:
- 成功生成了高分辨率的海平面曲线.
- 确定了持续的海平面振荡,其频率高于轨道强迫.
- 这些发现挑战了通过轨道变化的海平面变化的独家解释.
结论:
- 亚轨道频率的气候振荡显著影响海平面.
- 新的约会方法为古气候研究提供了更可靠的工具.
- 了解这些海平面快速变化对于预测未来气候影响至关重要.
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