相关实验视频
Updated: Jun 3, 2026

04:35
Preparation of Free-Surface Hyperbolic Water Vortices
Published on: July 28, 2023
在海洋前沿增强流和能量消耗
Eric D'Asaro1, Craig Lee, Luc Rainville
1Applied Physics Laboratory and School of Oceanography, University of Washington, Seattle, WA 98105-6698, USA. dasaro@apl.washington.edu
概括
海洋前沿可以显著激发海洋表面边界层的流,挑战大气强迫作为唯一驱动力的传统观点. 这一发现影响了气候模型和我们对空海交换的理解.
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:
- 海洋表面边界层 (OSBL) 对于空海交换至关重要.
- 传统上,大气强迫被认为是OSBL流的主要驱动因素.
- 当前的气候模型依赖于这个范式.
研究的目的:
- 调查导致OSBL流的能源.
- 挑战大气强迫的经典范式作为唯一的驱动力.
- 量化海洋前沿在OSBL流中的作用.
主要方法:
- 在Kuroshio流中1公里宽的前线的现场观测.
- 在OSBL中测量能量消耗率.
- 对风前方速度相互作用的定量分析.
主要成果:
- 观察到的能量消散率增大了一到两倍.
- 有证据表明海洋前沿,而不是大气强迫,为流提供了能量.
- 与正面速度对齐的风催化了从正面释放到流的能量.
- 由此产生的边界层是分层的,与经典的混合良好的层不同.
结论:
- 海洋前沿可以成为OSBL流动的主要能源.
- 这一发现需要对气候模型和空海交换参数进行修订.
- 主流 (库罗西奥,墨西哥湾流,ACC) 的强烈前线对气候有重大影响.
相关概念视频
Turbulent Flow
Turbulent flow is characterized by unpredictable fluctuations in velocity and pressure, which result in a chaotic fluid movement distinct from the orderly patterns of laminar flow. While laminar flow is governed by smooth, parallel layers with minimal mixing, turbulent flow exhibits highly irregular, three-dimensional patterns. This behavior arises due to instabilities in the fluid's velocity profile, and amplifies as the flow velocity increases. Minor disturbances, known as turbulent spots,...
Boundary Layer Characteristics
When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
Laminar Flow
Laminar flow represents a smooth, orderly fluid motion where particles move along parallel paths, resulting in minimal mixing between layers. Streamlined particle paths characterize this flow regime and occur under conditions where viscous forces dominate over inertial forces. The distinction between laminar, transitional, and turbulent flow is primarily determined by the Reynolds number, a dimensionless quantity calculated as:
Damped Oscillations
In the real world, oscillations seldom follow true simple harmonic motion. A system that continues its motion indefinitely without losing its amplitude is termed undamped. However, friction of some sort usually dampens the motion, so it fades away or needs more force to continue. For example, a guitar string stops oscillating a few seconds after being plucked. Similarly, one must continually push a swing to keep a child swinging on a playground.
Although friction and other non-conservative...
Although friction and other non-conservative...
Energy Considerations in Open Channel Flow
Open channel flow, where a fluid flows with a free surface exposed to the atmosphere, is primarily governed by gravitational and surface effects, distinguishing it from closed conduit or pipe flow. In open channels such as rivers, canals, and artificial channels, energy analysis provides valuable insights into flow behavior and the relationship between depth, velocity, and slope.Specific Energy and Flow DepthIn open channel flow, the specific energy, E, combines the gravitational potential...
General External Flow Characteristics
The study of external flow is essential for creating structures and objects that interact efficiently and safely with moving fluids, such as air or water. When a body is immersed in a flowing fluid, it experiences two primary forces: drag, which opposes motion along the flow direction, and lift, which acts perpendicular to the flow. The shape, size, and orientation of the object influence these forces.Streamlined and Blunt Bodies in External FlowObjects in fluid flow are classified as...

