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一个供应有限的洪流,不感受到气候变化的热量
Jiazhi Qie1, Adrien Favillier2,3, Frédéric Liébault4
1Climatic Change Impacts and Risks in the Anthropocene (C-CIA), Institute for Environmental Sciences, University of Geneva, 66 Boulevard Carl Vogt, CH-1205, Geneva, Switzerland. jiazhi.qie@etu.unige.ch.
Nature communications
|October 21, 2024
概括
气候变暖可能会改变阿尔卑斯山的碎片流,但长期记录很少. 对瑞士废物流系统进行的400年研究没有发现频率或规模的重大变化,这表明沉积物供应,而不是气候,驱动活动.
科学领域:
- 地质科学 地质科学
- 气候科学 气候科学
- 自然危害 自然危害
背景情况:
- 由于气候变暖,阿尔卑斯山的碎片流活动预计将发生变化.
- 评估这些变化的一个重大挑战是缺乏长期碎片流记录.
- 了解碎片流动的动态对于危险和风险评估至关重要.
研究的目的:
- 重建瑞士东部阿尔卑斯山最长的连续碎片流时间序列.
- 调查气候变化对碎片流动频率和规模的影响.
- 在供应有限的系统中分析控制碎片流动启动的因素.
主要方法:
- 使用树环分析重建400年 (1626-2020) 的碎片流记录.
- 分析了Multetta现场因碎片流而损坏的树木生长环.
- 对碎片流动频率,大小和休息时间模式的统计分析.
主要成果:
- 该研究为阿尔卑斯山 (1626-2020年) 建立了最长的连续碎片流记录.
- 在400年的时间里,没有发现碎片流动频率或规模的显著变化.
- 碎片流的启动似乎主要是由沉积物供应和充电控制的,而不是直接的气候影响.
结论:
- 在这个供应有限的系统中,尽管气候波动,但碎片流活动在几个世纪以来表现出了显著的稳定性.
- 这些发现与由于气候变暖而导致碎片流动活动增加的预期形成鲜明对比.
- 沉积物动态对于了解碎片流动行为和高山环境中的危险评估至关重要.
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