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Updated: May 5, 2026

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
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在北冰洋中风通循环制度的早期米奥森开始
Martin Jakobsson1, Jan Backman, Bert Rudels
1Department of Geology and Geochemistry, Stockholm University, SE-106 91 Stockholm, Sweden. martin.jakobsson@geo.su.se
Nature
|June 22, 2007
概括
北极海洋大约在1750万年前由于弗拉姆海峡的开放而变得完全有氧化. 这一事件显著影响了全球的热环流和气候.
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:
- 北极和北大西洋的深水形成推动了全球的热盐环流和气候.
- 来自北极地区的有限的纪沉积物核心数据阻碍了对其循环历史的理解.
- 北极和北大西洋之间的深水交换的时间仍然受到很小的限制.
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