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Updated: Apr 28, 2026

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
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古海洋学.古海洋学. 地中海外流开始流入北大西洋
F Javier Hernández-Molina1, Dorrik A V Stow2, Carlos A Alvarez-Zarikian3
1Department of Earth Sciences, Royal Holloway, University of London, Egham, Surrey TW20 0EX, UK. javier.hernandez-molina@rhul.ac.uk.
概括
地中海外流水 (MOW) 循环对北大西洋气候变化产生了重大影响. 与构造事件相关的MOW体积增加影响了热环流和大西洋南部翻转环流 (AMOC).
科学领域:
- 海洋学 海洋学 海洋学
- 古海洋学是古海洋学.
- 气候科学 气候科学
背景情况:
- 地中海外流水 (MOW) 是影响大西洋循环的重要水体.
- 了解其历史变异性对于重建过去的气候动态至关重要.
研究的目的:
- 重建地中海外流水 (MOW) 循环模式,从世到现在.
- 研究MOW对全球热环流 (THC) 和大西洋南部翻转环流 (AMOC) 的影响.
主要方法:
- 从综合海洋钻井计划探险339号探险队西南伊比利亚边缘沿线的沉积物分析.
- 识别沉积间隙,表明底部电流侵蚀.
主要成果:
- 在533万年前,直布罗陀海峡开放后,有限的MOW进入了大西洋.
- 从普略纪晚期开始,MOW数量的增加导致了侵蚀性间隙.
- 这些间隙与区域构造事件和全球热环流 (THC) 变化相关.
结论:
- MOW在影响AMOC,THC和气候变化方面发挥了关键作用.
- MOW为北极度提供了温暖的盐水.
- MOW的循环反过来又受到板块构造学的影响.
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