概括
格陵兰冰盖在3万年前之前已经超过了100公里,超过了目前的边缘. 高北极地区威斯康星州晚期有限的冰面范围表明由于劳伦提德冰盖造成的极端干旱.
科学领域:
- 冰川学的冰川学
- 四年纪地质学四年纪地质学
- 北极古气候学 古气候学
背景情况:
- 埃尔塞梅尔岛的实地观测提供了对过去冰盖动态的洞察.
- 了解冰盖的行为对于预测未来气候变化影响至关重要.
研究的目的:
- 重建西北格陵兰冰盖和埃尔塞米尔岛的冰川历史.
- 为了确定冰的前进和撤退的时间和程度.
- 调查影响高北极冰盖行为的环境条件.
主要方法:
- 在埃尔塞默岛东北部进行现场观测和地质测绘.
- 放射性碳测年法用于建立时间框架 (在现在之前的几年).
- 对冰盖边缘和冰后地形证据的分析.
主要成果:
- 西北格陵兰冰盖超过100公里超出了目前的边缘.
- 这一重大进步早于埃尔斯米尔岛最外围的冰川进步 (>公元前3万年). ) 的情况.
- 经济衰退开始于公元28000年至3万年之间. (可能>35,000年 B.P. B.P. ),威斯康星州晚期冰面范围有限,无冰走廊.
结论:
- 显著的无冰区在冰川时期仍然存在.
- 威斯康星州晚期冰在高北极地区的有限范围可能是由极端干旱造成的.
- 干旱是劳伦提德冰盖向南积累的结果.
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