相关实验视频
Updated: May 7, 2026

08:01
The Diffusion of Passive Tracers in Laminar Shear Flow
Published on: May 1, 2018
快速交叉密度海洋在德雷克海峡中部深度混合,通过追踪器释放测量
Andrew J Watson1, James R Ledwell, Marie-José Messias
1School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich NR4 7TJ, UK. andrew.watson@exeter.ac.uk
Nature
|September 20, 2013
概括
对于海洋循环至关重要,由于海底地形粗,在德雷克海峡显著增强了对平面的混合. 这一发现有助于解释深海水如何返回表面.
科学领域:
- 海洋学 海洋学 海洋学
- 流体动力学 流体动力学
- 气候科学 气候科学
背景情况:
- 对于全球海洋翻转循环来说,二氧化的混合是必不可少的.
- 内部海洋混合不足以平衡全球循环.
- 在地形"热点"中接近底部的混合部分弥补了这一缺口.
研究的目的:
- 为了调查在中深层的二氧化混合的程度和驱动因素.
- 为了确定德雷克海峡在海洋翻转循环中的作用.
- 量化跨密度混合对南大洋上游的贡献.
主要方法:
- 使用三甲基硫黄五化物在公海释放的追踪剂.
- 测量跨密度表面的介质混合率.
- 南极环极电流的分析与德雷克海峡地形的相互作用.
主要成果:
- 在德雷克海峡中观测到中深水域的二氧化混合量持续增加了20倍.
- 由南极环极电流在粗的地形上产生的流被确定为原因.
- 观察到的混合与20 sverdrup (Sv) 南部部件相容,以全球翻转.
结论:
- 在德雷克海峡,粗的海底地形显著增强了形混合.
- 这一地区的交叉密度混合在很大程度上 (20-30%) 导致南大洋上游.
- 这个过程是全球海洋颠覆循环的关键组成部分.
更多相关视频
相关概念视频
Uniform Depth Channel Flow
Uniform depth channel flow keeps fluid depth consistent along channels such as irrigation canals. In natural channels, such as rivers, approximate uniform flow is often assumed. This condition occurs when the channel’s bottom slope matches the energy slope, balancing potential energy lost from gravity with head loss due to shear stress. This balance prevents depth changes along the channel length, resulting in a steady, uniform flow.Uniform flow in open channels with a constant cross-section...
Drift Velocity
The high speed of electrical signals results from the fact that the force between charges acts rapidly at a distance. Thus, when a free charge is forced into a wire, the incoming charge pushes other charges ahead due to the repulsive force between like charges. These moving charges move the charges farther down the line. The density of charge in a system cannot easily be increased, so the signal is passed on rapidly. The resulting electrical shock wave moves through the system at nearly the...
Deep Sea Microbial Ecology
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...

