来自喜马拉雅山脉冰芯的南亚季风的高分辨率千年记录
Thompson1, Yao, Mosley-Thompson
1Byrd Polar Research Center, The Ohio State University, Columbus, OH 43210, USA. Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou China. Department of Geological Sciences, Department of Geography,
概括
一个西藏冰芯揭示了南亚季风.
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:
- 冰芯提供了宝贵的古气候记录.
- 西藏高原对南亚季风的变化敏感.
研究的目的:
- 用Dasuopu,西藏的高分辨率冰芯记录重建过去的南亚季风强度.
- 调查20世纪人类活动对区域气候的影响.
主要方法:
- 对来自西藏达苏普的冰芯中的尘埃和化物度的分析.
- 冰芯部分的高分辨率约会. 冰芯部分的高分辨率约会.
- 与历史气候数据和区域人类活动的比较.
主要成果:
- 达苏普冰芯对南亚季风波动敏感,尘埃和化物水平表明干旱的强度.
- 记录下来的最严重的干旱发生在公元1790年至1796年之间.
- 20世纪尘埃和化物度的显著增加反映了印度和尼泊尔的人类活动的增加.
- 证据表明,整个高原的20世纪变暖趋势,在更高的海拔地区放大,与其他西藏冰芯相一致.
结论:
- 达苏普冰芯提供了过去季风变化和干旱事件的详细记录.
- 20世纪该地区的气候变化与增加的人类活动密切相关.
- 西藏高原正在经历放大变暖,这对区域水文和生态系统有影响.
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