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秘鲁安第斯山脉的Holocene冰川波动表明北方气候联系
Joseph M Licciardi1, Joerg M Schaefer, Jean R Taggart
1Department of Earth Sciences, University of New Hampshire, Durham, NH 03824, USA. joe.licciardi@unh.edu
热带冰川揭示了秘鲁早期的全新世和小冰河时代的气候变化. 这些发现表明热带气候与北大西洋地区有关,挑战了以前的假设.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 气候科学 气候科学
背景情况:
- 热带地区在全球气候动态中的作用受到辩论.
- 热带冰川记录对于了解区域气候至关重要,但缺乏精确的日期.
研究的目的:
- 为了建立在秘鲁维尔卡班巴山脉的冰川事件的精确时间表.
- 调查热带气候与其他地区的联系.
主要方法:
- 使用地质年代学技术,精确地测定了摩林的年代.
- 对热带外部冰川波动的分析.
主要成果:
- 识别了早期Holocene和晚期小冰河时代的突出冰川事件.
- 为秘鲁南部开发了强大的冰川时间表.
- 与新西兰冰川记录相比,观察到的差异.
结论:
- 热带冰川的波动表明热带外部气候发生了重大气候变化.
- 秘鲁的冰川记录与欧洲的记录相关,这表明北大西洋的气候联系.
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