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相关概念视频

Hydraulic Jump01:29

Hydraulic Jump

263
A hydraulic jump is a sudden rise in fluid depth in open channels, occurring when high-velocity (supercritical) flow transitions to low-velocity (subcritical) flow. This phenomenon requires an upstream Froude number greater than 1, as flows with Fr1<1 remain subcritical, making a hydraulic jump impossible due to the need for negative head loss, which violates thermodynamic principles.The characteristics of a hydraulic jump depend on the upstream Froude number and are classified as...
263
Hydraulic Jump: Problem Solving01:16

Hydraulic Jump: Problem Solving

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To analyze a hydraulic jump in a rectangular channel with a flow speed of 6 meters per second, follow these steps:Calculate Effective Upstream Velocity:When the downstream gate closes, a hydraulic jump forms, traveling upstream at 2 meters per second. This wave speed combines with the initial channel flow velocity, creating an effective upstream velocity.Identify Flow Velocities Before and After the Hydraulic Jump:Upstream of the hydraulic jump, the effective flow velocity includes both the...
216
Precipitation Processes01:12

Precipitation Processes

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The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
947
Excess Pressure Inside a Drop and a Bubble01:13

Excess Pressure Inside a Drop and a Bubble

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The shape of a small drop of liquid can be considered spherical, neglecting the effect of gravity. This drop can further be considered as two equal hemispherical drops put together due to surface tension. The forces acting on the spherical drop are due to the pressure of the liquid inside the drop, the pressure due to air outside the drop, and the force due to the surface tension acting on the two hemispherical drops.
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Shock Waves01:16

Shock Waves

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While deriving the Doppler formula for the observed frequency of a sound wave, it is assumed that the speed of sound in the medium is greater than the source's speed through it. When this condition is breached, a shock wave occurs.
When the source's speed approaches the speed of sound, constructive interference between successive wavefronts emitted by the source occurs immediately behind it. Initially, scientists believed that this constructive interference would result in such high...
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Design Example: Creating a Hydraulic Model of a Dam Spillway01:21

Design Example: Creating a Hydraulic Model of a Dam Spillway

392
Scaled hydraulic models of dam spillways provide a practical way to replicate and study the intricate flow dynamics of these structures. Often built to a 1:15 ratio, these models allow for observing critical water behavior, such as velocity distribution, flow patterns, and energy dissipation.
392

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Spaceborne Cloud and Precipitation Radars: Status, Challenges, and Ways Forward.

Reviews of geophysics (Washington, D.C. : 1985)·2020
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相关实验视频

Updated: Oct 20, 2025

Visualization of High Speed Liquid Jet Impaction on a Moving Surface
08:34

Visualization of High Speed Liquid Jet Impaction on a Moving Surface

Published on: April 17, 2015

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在超级电池雷暴上方的液压跳动力学

Morgan E O'Neill1, Leigh Orf2,3, Gerald M Heymsfield3,4

  • 1Department of Earth System Science, Stanford University, Stanford, CA 94305, USA.

Science (New York, N.Y.)
|September 13, 2021
PubMed
概括

最强烈的雷暴通过像山一样的行为,在平流层中注入大量的水蒸气,从而创造了杆上方的圆柱体 (AACP). 这一过程影响了臭氧和气候.

科学领域:

  • 大气科学
  • 天气学
  • 气候科学

背景情况:

  • 上方的形 (AACP) 与强大的超级电池雷暴有关.
  • 在臭氧层消耗和全球变暖方面, AACP 的平流层水分作用尚不清楚.
  • 了解AACP的形成对于气候建模至关重要.

研究的目的:

  • 为了研究上方的形羽毛的物理机制.
  • 通过超级细胞量化平流层水蒸气注入的潜力.

主要方法:

  • 使用大型模拟来建模AACP形成.
  • 通过雷达观察证实了模拟结果.
  • 分析了超射对流和平流层流之间的相互作用.

主要成果:

  • 一个超级电池的超射顶部作为一个地形障碍.
  • 一个液压跳跃形成在热带,类似于山脉诱导的风暴.
  • 模拟向平流层注入的水蒸气可以超过每秒7.

结论:

  • 这项研究阐明了通过热带液跳跃生成AACP的机制.

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  • 超级电池雷暴可以显著地给平流层提供水分.
  • 这些发现突出了影响平流层化学和气候的关键过程.