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在过去的1800年里,每年解决的冰芯记录了热带气候变化
L G Thompson1, E Mosley-Thompson, M E Davis
1Byrd Polar Research Center, The Ohio State University, Columbus, OH 43210, USA. thompson.3@osu.edu
概括
来自秘鲁奎尔卡亚冰盖的高分辨率冰芯揭示了1800年的热带气候变化. 这些记录将氧同位素与海面温度,/酸盐与热带融合区迁移联系起来.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 热带气候的动力学
背景情况:
- 低度的冰芯提供了独特的热带气候见解,但很少.
- 秘鲁的Quelccaya冰盖是一个关键的,但尚未充分利用的,过去气候的档案.
研究的目的:
- 从Quelccaya冰盖重建了过去1800年的高分辨率气候变化.
- 将冰芯代理数据与热带安第斯和太平洋的特定气候驱动因素联系起来.
主要方法:
- 从Quelccaya每年解决的冰芯记录的分析.
- 测量氧同位素比率 (δ(18) O) 用于海面温度的重建.
- 量化和酸盐度以追踪热带融合区 (ITCZ) 的迁移.
主要成果:
- 冰芯提供了1800年的气候变化记录,每年的分辨率.
- 氧同位素与热带东太平洋海洋表面温度相关.
- 和酸盐度反映了ITCZ迁移对热带安第斯山脉的重大影响.
结论:
- 奎尔卡亚冰盖是了解长期热带气候动态的重要档案.
- 过去的ITCZ迁移模式在冰核记录中得到了明确记录.
- 冰盖目前的撤退表明它比至少6000年来更小.
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