尘埃:在最后一个冰川最大时期的水文循环的诊断
1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena 91125, USA.
概括
在最后的冰川最大期 (LGM) 期间的高尘埃度表明水文循环较弱. 这一发现与该时期海洋温度显著降低的证据一致.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 海洋学 海洋学 海洋学
背景情况:
- 来自格陵兰岛和南极洲的冰芯显示,在最后的冰川最大期 (LGM) 期间,尘埃度升高.
- 以前的研究表明,在LGM期间,全球气候显著降温.
研究的目的:
- 为了解释在LGM冰芯中观察到的高尘埃度.
- 调查LGM期间尘埃水平,水文周期强度和海洋温度之间的关系.
主要方法:
- 分析冰芯中的尘埃度.
- 模拟水文循环的强度.
- 从珊瑚记录中解释古海洋学数据 (石和测量).
主要成果:
- 在LGM冰芯中观察到的尘埃增强与水文循环相一致,水文循环大约比当今水平弱50%.
- 这种降低水文周期强度与LGM期间海洋温度大幅下降 (约5°C) 相相关.
结论:
- 与当前相比,LGM经历了一个明显较弱的水文周期.
- 降低的海洋温度可能在LGM期间起到了调节水文循环和大气尘埃运输强度的作用.
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