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北大西洋气候在最后一个冰川最大期的多世纪变化模式
Matthias Prange1, Lukas Jonkers1, Ute Merkel1
1MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.
Science advances
|November 1, 2023
概括
在最后的冰川最大期 (LGM) 期间,北大西洋的温度在几个世纪内变化比今天更多. 一个新的气候模型模拟显示了由海洋循环和盐度驱动的自我持续的振荡,解释了这种增加的古气候变化.
科学领域:
- 古气候学 古气候学
- 气候动力学 气候动力学
- 海洋学 海洋学 海洋学
背景情况:
- 古气候记录显示,北大西洋在最后一个冰川最大期 (LGM) 中的多世纪温度变化比当前的冰川间更大.
- 在类似的外部强迫下,这种放大古气候变化的驱动因素仍然不太清楚.
研究的目的:
- 调查北大西洋地区LGM期间增强的多世纪温度变化的原因.
- 在LGM条件下识别和描述气候变化的新模式.
主要方法:
- 为了LGM,利用了全面的合气候模型模拟.
- 从北大西洋地区集成的高分辨率古气候代理记录.
- 分析了与大西洋南部翻转循环 (AMOC) 和盐度相关的振荡模式的变化.
主要成果:
- 引入了LGM独特的多世纪变化的自我维持的振荡模式.
- 这种模式是由适度的AMOC变化和大规模的盐分分布驱动的,由海冰反放大.
- 在亚极北大西洋中观察到最大的表面温度变化,与Dansgaard-Oeschger事件不同.
结论:
- 确定了多个世纪的振荡解释了LGM期间古气候温度变化增加.
- 这种模式是LGM强迫的特征,并且与其他气候振荡有动态差异.
- 在不断变化的气候强迫下,这种变化模式的出现和消失对未来的气候变化预测有影响.
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