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由热带远程连接引发的长达一个世纪的西南极雪积累变化
Kai Man1,2, Jürg Luterbacher3, David M Holland4
1Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China.
Science advances
|January 29, 2025
概括
热带海洋的变化推动了20世纪南极的降雪趋势. 这种热带-极地远程连接增加了南极冰层,影响了全球海平面.
科学领域:
- 气候科学 气候科学
- 冰川学的冰川学
- 海洋学 海洋学 海洋学
背景情况:
- 冰芯数据显示,在20世纪期间,南极洲西部的积雪趋势相反.
- 现有的文献缺乏关于热带海洋和极地之间的百年级远程连接的研究.
研究的目的:
- 研究热带海洋变化对南极长期降雪模式的影响.
- 为了识别和描述热带和南极之间的百年级远程连接.
主要方法:
- 冰芯数据和气候记录的统计分析.
- 数字实验模拟热带-极地相互作用.
主要成果:
- 热带大西洋的变暖和赤道太平洋的降温显著改变了向西南极洲的水分传输.
- 一个双极状的降雪模式出现,南极半岛/埃尔斯沃思陆地积雪量增加,玛丽·伯德陆地积雪量减少.
- 确定了热带海洋变化和南极降雪之间的百年级远程连接.
结论:
- 热带海洋变化是20世纪南极降雪趋势的主要驱动因素.
- 这种热带-极地联系有助于增加南极冰质量,部分抵消冰架薄化和影响全球海平面.
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