冰川在年轻的干旱和8.2ka事件期间在巴芬岛,加拿大北极地区的冰川范围
Nicolás E Young1, Jason P Briner, Dylan H Rood
1Department of Geology, University at Buffalo, 411 Cooke Hall, Buffalo, NY 14260, USA. nicolasy@ldeo.columbia.edu
概括
8.2ka冷事件导致巴芬岛,加拿大北极地区的冰川大幅进步,山地冰川超过了年轻的德里亚斯大小. 这表明与较年轻的干旱相比,不同的季节性冷却模式.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 四分学科学 四分学科学
背景情况:
- 格陵兰岛的冰芯表明年轻的德里亚斯 (YD) 和8.2ka的寒冷事件明显比现在更冷.
- 了解冰盖和冰川对过去气候变化的反应对于预测未来冰盖的敏感性至关重要.
研究的目的:
- 重建洛伦蒂德冰盖和巴芬岛山脉冰川对8.2ka气候事件的反应.
- 为了比较冰川在8.2ka事件中的行为与年轻的Dryas.
主要方法:
- 对冰芯进行分析,以获取古气候数据.
- 重建冰盖出口冰川和巴芬岛上的山地冰川的延伸.
主要成果:
- 劳伦蒂德冰盖出口冰川和巴芬岛山冰川的广泛前进发生在对8.2ka事件的反应中.
- 在8.2ka事件期间的山地冰川比年轻德里亚斯时期的冰川更大.
- 在8.2ka事件期间的冷却可能比冬季偏差的YD冷却更为季节均.
结论:
- 8.2ka事件引发了大量的冰川扩张,表明冰盖和冰川对气候扰乱的敏感性很大.
- 观测到的冰川动态和季节性温度分布为我们提供了早期全新世纪地区气候变化的洞察力.
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