在最后一个冰川结束期间,北太平洋的深水形成
Y Okazaki1, A Timmermann, L Menviel
1Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
概括
在最后的冰川终结期间,北大西洋循环减弱,导致深水形成转移到北太平洋. 这种海洋循环变化调节了全球热传输.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋学 海洋学 海洋学
背景情况:
- 大西洋南部翻转循环 (AMOC) 在17,50015,000年前由于北半球冰盖融水而显著减弱.
- 这种AMOC减弱产生了全球影响,影响了南极洲和北太平洋.
研究的目的:
- 为了调查北太平洋在最后一次冰川终结期间深水形成中的作用.
- 了解海洋热传输变化的全球影响.
主要方法:
- 分析北太平洋古老地表代理数据.
- 编制海洋放射性碳年龄通风记录.
- 全球气候模型模拟.
主要成果:
- 证据表明,在最后一个冰川结束的早期,北太平洋的深水形成发生在25003000米的深度.
- 在北大西洋和北太平洋之间发生了深水形成位置的显著转换.
结论:
- 北太平洋在这个时期对深水形成起到了至关重要的作用.
- 观察到的深水形成的开关是调节极向海洋热传输的关键,在整个最后一次冰川终结期间.
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