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相关概念视频

Buoyancy00:59

Buoyancy

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When an object is placed in a fluid, it either floats or sinks. All objects in a fluid experience a buoyant force. For example, a metal ball sinks, while a rubber ball floats. Similarly, a submarine can sink and float by adjusting its buoyancy.  The concept of buoyancy raises several interesting questions. For instance, where does this buoyant force come from? How much buoyant force is required to make an object sink or float? Do objects that sink get any support at all from the...
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Archimedes' Principle01:13

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Archimedes' principle states that an upward buoyant force exerted on a body that is immersed partially or entirely in a fluid is equal to the weight of the fluid displaced by it. To understand how much buoyant force is needed to make an object float, let us think about what happens when a submerged object is removed from a fluid. If the object were not in the fluid, the space occupied by the object would be filled by the fluid having a weight wfl. This weight is supported by the...
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Buoyancy and Stability for Submerged and Floating Bodies01:11

Buoyancy and Stability for Submerged and Floating Bodies

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In fluid mechanics, buoyancy and stability are key concepts for understanding the behavior of submerged and floating bodies. When a stationary body is fully or partially submerged in a fluid, the fluid exerts a force on the body known as the buoyant force. This force acts vertically upward through a point called the center of buoyancy, which is the center of the displaced fluid volume. According to Archimedes' principle, the magnitude of the buoyant force is equal to the weight of the fluid...
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Tidal Forces01:06

Tidal Forces

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The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to...
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Hydrostatic Pressure Force on a Plane Surface01:04

Hydrostatic Pressure Force on a Plane Surface

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When a plane surface is submerged in a fluid, hydrostatic forces develop on the surface due to the fluid's pressure. For horizontal surfaces, the pressure exerted by the fluid is uniform because the depth remains constant. The resultant force is determined by the pressure at the given depth multiplied by the area of the surface, and it acts through the centroid of the surface. For vertical surfaces, the pressure varies with depth, increasing as the distance from the fluid's free surface...
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Surface Tension of Fluid01:22

Surface Tension of Fluid

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Surface tension is a fundamental property of fluids, occurring at the boundary between a liquid and a gas or between two immiscible liquids. This phenomenon arises from the cohesive forces between molecules at the fluid's surface, creating an effect similar to a stretched elastic membrane. Inside each fluid, molecules are equally attracted in all directions by neighboring molecules, but surface molecules experience a net inward force, resulting in surface tension.
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相关实验视频

Updated: Sep 15, 2025

Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing
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Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing

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降雨是否会在海洋表面产生浮力力?

Dipanjan Chaudhuri1, Eric A D'Asaro2,3

  • 1Applied Physics Laboratory, University of Washington, 1013 NE 40th Street, Seattle, 98105-6698, WA, USA. dipadadachaudhuri@gmail.com.

Nature communications
|July 15, 2025
PubMed
概括
此摘要是机器生成的。

降雨对海洋浮力的影响是复杂的. 轻雨会破坏海洋的稳定,而大雨则会使海洋稳定,这挑战了关于降水对海洋表面层的影响的假设.

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Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
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Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

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Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
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相关实验视频

Last Updated: Sep 15, 2025

Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing
08:54

Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing

Published on: February 13, 2018

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Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
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Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
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科学领域:

  • 海洋学 海洋学 海洋学
  • 大气科学 大气科学
  • 气候科学 气候科学

背景情况:

  • 降雨通过淡水流和冷却效应影响上层海洋浮力.
  • 海洋表面的稳定性对海洋生态系统和气候调节至关重要.

研究的目的:

  • 在各种降雨条件下,量化赤道海洋的净浮力流.
  • 为了研究与降雨相关的浮力流的日间变异性.

主要方法:

  • 在现场测量浮力流动,使用22个挂泊浮标.
  • 数据的分类基于降雨强度 (轻与重) 和白天时间 (白天与夜晚).

主要成果:

  • 轻雨 (0.2-4毫米/小时) 通常会破坏海洋表面的稳定.
  • 大雨 (>4毫米/小时) 倾向于稳定海洋表面.
  • 与白天降雨相比,夜间降雨导致海洋不稳定的可能性是白天降雨的两倍,无论强度如何.

结论:

  • 降雨对海洋浮力的影响并非均稳定.
  • 降雨量的日间变化显著影响海洋表面的稳定性.
  • 这些发现挑战了关于降水的传统观点,认为降水仅仅是对海洋的稳定力.