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Updated: Jun 10, 2025

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
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三层循环在世界上最深的状沟
Huichang Jiang1, Xiao Xin2, Hongzhou Xu3
1Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, China.
Nature communications
|October 17, 2024
概括
挑战者深处的海洋流显示出三层循环模式. 这一发现澄清了深海动态和海洋盆地之间的连接.
科学领域:
- 海洋学 海洋学 海洋学
- 深海勘探是深海的探索.
- 流体动力学 流体动力学
背景情况:
- 挑战者深度 (CD) 是世界上最深的海底沟.
- 由于在极深处的采样挑战,人们对CD中的海洋循环和水质运输的了解很少.
研究的目的:
- 研究挑战者深处的海洋循环结构和下环极深水 (LCDW) 运输.
- 为了阐明影响深海水力动力学因素的因素.
主要方法:
- 在挑战者深处部署一个超深的电流测量器泊位阵列.
- 分析收集的海洋学数据,以确定当前的模式和水质运动.
主要成果:
- 在CD中发现了一个独特的三层循环系统.
- 这些层由向西的LCDW流,旋风循环和反旋风循环组成.
- 西向的流量呈现季节性逆转,表明双向深海盆地连接.
结论:
- 三层循环是由LCDW入侵,局部地形和流混合调节的.
- 流混合是反旋风循环的关键驱动力.
- 这些发现增强了对地球最深的海洋区域水力动力学环境的理解.
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