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関連する概念動画

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...
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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...
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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

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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.
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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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関連する実験動画

Updated: Oct 20, 2025

Visualization of High Speed Liquid Jet Impaction on a Moving Surface
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Visualization of High Speed Liquid Jet Impaction on a Moving Surface

Published on: April 17, 2015

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スーパーセル雷雨の上の水力ジャンプダイナミクス

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
まとめ
この要約は機械生成です。

最も強い雷雨は,山のように振る舞い,高層圏に水蒸気を注入することで,上方アンビルシルス羽根 (AACP) を生み出します. このプロセスはオゾンと気候に 影響を及ぼします

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A Microfluidic System with Surface Patterning for Investigating Cavitation Bubble(s)&#8211;Cell Interaction and the Resultant Bioeffects at the Single-cell Level
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A Microfluidic System with Surface Patterning for Investigating Cavitation Bubble(s)–Cell Interaction and the Resultant Bioeffects at the Single-cell Level

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Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
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関連する実験動画

Last Updated: Oct 20, 2025

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A Microfluidic System with Surface Patterning for Investigating Cavitation Bubble(s)&#8211;Cell Interaction and the Resultant Bioeffects at the Single-cell Level
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Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
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科学分野:

  • 大気科学
  • 気象学
  • 気候科学

背景:

  • 強い超細胞雷雨に結びついている.
  • AACPからの平流層の水分は,オゾン層の減少と地球温暖化に不明な役割を果たしています.
  • AACPの形成を理解することは 気候モデリングに不可欠です

研究 の 目的:

  • 円柱状の羽根形成の背後にある物理的メカニズムを調査する.
  • スーパーセルによる平流層の水蒸気注入の可能性を定量化するために.

主な方法:

  • AACPの形成をモデル化するために大きな渦のシミュレーションを使用しました.
  • レーダー観測で実証されたシミュレーション結果
  • オーバーシューティングコンベクションと ストラトスフィアの流れの相互作用を分析した.

主要な成果:

  • スーパーセルの上部が 地形上の障害物として機能します
  • 熱帯圏で発生する水力ジャンプは 山脈で発生する風の嵐に似ています
  • 準層への水蒸気注入のシミュレーションは,毎秒7トンを超えます.

結論:

  • この研究は,トロポパウスの水力ジャンプによるAACP生成のメカニズムを明らかにしています.
  • 超細胞雷雨は 低層圏をかなり水分化する
  • この発見は,平流圏の化学と気候に影響を与える 重要な過程を強調しています