全新纪 - - 晚期普莱斯托纪气候冰芯记录来自青海-西藏高原
概括
来自中国德冰盖的气候记录显示,晚期冰川阶段更冷,更潮湿. 最近几十年是最温暖的几十年之一,与全新世纪最大值相匹配.
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:
- 冰芯提供了过去气候状况的宝贵档案.
- 青海-西藏高原是理解亚洲气候动态的关键地区.
研究的目的:
- 为了重建Holocene和Late Glacial Stage (LGS) 期间的亚热带气候变化.
- 为了比较LGS的气候条件与Holocene时代的气候条件.
主要方法:
- 分析了三个深层冰芯,这些冰芯在德冰盖的岩基上钻孔.
- 检查同位素组成 (delta(18) O),灰尘含量,可溶性气溶和冰晶大小.
主要成果:
- 晚期冰川阶段的条件与全新纪相比,其特点是温度较低,降水量增加和尘埃水平较高.
- 度,尘埃度,可溶性气溶和冰晶大小的显著变化标志着从LGS过渡到Holocene.
- 这些快速的气候变化发生在大约1万年前.
- 过去的60年是整个冰核记录中最温暖的时期之一,与全新世热量最大值相当.
结论:
- 德冰盖的冰芯为过去数万年的亚热带气候变化提供了详细的代理.
- 在最后一个冰川时期结束时,气候发生了快速变化,影响了该地区的气候.
- 最近的变暖趋势凸显了当前气候系统的重大变化.
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