Jove
Visualize
お問い合わせ
JoVE
x logofacebook logolinkedin logoyoutube logo
JoVEについて
概要リーダーシップブログJoVEヘルプセンター
著者向け
出版プロセス編集委員会範囲と方針査読よくある質問投稿
図書館員向け
推薦の声購読アクセスリソース図書館諮問委員会よくある質問
研究
JoVE JournalMethods CollectionsJoVE Encyclopedia of Experimentsアーカイブ
教育
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab Manual教員リソースセンター教員サイト
利用規約
プライバシーポリシー
ポリシー

関連する概念動画

Tidal Forces01:06

Tidal Forces

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 black holes.
Modes of Standing Waves - I01:03

Modes of Standing Waves - I

A close look at earthquakes provides evidence for the conditions appropriate for resonance, standing waves, and constructive and destructive interference. A building may vibrate for several seconds with a driving frequency matching the building's natural frequency of vibration; this produces a resonance that results in one building collapsing while the neighboring buildings do not. Often, buildings of a certain height are devastated, while other taller buildings remain intact. This phenomenon...
Modes of Standing Waves: II01:04

Modes of Standing Waves: II

The starting point for expressing the modes of standing waves is understanding the boundary conditions that the waves must follow. The boundary conditions are derived from the physical understanding of how the standing waves are sustained, that is, how the vibrating particles of the medium behave at the boundaries imposed on them.
For a tube open at one end and closed at the other filled with air, the modes are such that there is always an antinode at the open end and a node at the closed end.
Standing Waves01:17

Standing Waves

Sometimes waves do not seem to move; rather, they just vibrate in place. Unmoving waves can be seen on the surface of a glass of milk kept in a refrigerator, which is one example of standing waves. Vibrations from the refrigerator motor create waves on the milk that oscillate up and down but do not seem to move across the surface. These waves are formed or created by the superposition of two or more identical moving waves in opposite directions. The waves move through each other, with their...
Wave Parameters01:10

Wave Parameters

The simplest mechanical waves are associated with simple harmonic motion and repeat themselves for several cycles. These simple harmonic waves can be modeled using a combination of sine and cosine functions. Consider a simplified surface water wave that moves across the water's surface. Unlike complex ocean waves, in surface water waves, water moves vertically, oscillating up and down, whereas the disturbance of the wave moves horizontally through the medium. If a seagull is floating on the...
Torsional Pendulum01:09

Torsional Pendulum

A torsional pendulum involves the oscillation of a rigid body in which the restoring force is provided by the torsion in the string from which the rigid body is suspended. Ideally, the string should be massless; practically, its mass is much smaller than the rigid body's mass and is neglected.
As long as the rigid body's angular displacement is small, its oscillation can be modeled as a linear angular oscillation. The amplitude of the oscillation is an angle. The role of mass is played by the...

こちらも読む

関連記事

共著者、ジャーナル、引用グラフによってこの研究に関連する記事。

並び替え
Same author

North atlantic ocean: preliminary description of normal modes.

Science (New York, N.Y.)·1972
関連記事をすべて見る

関連する実験動画

Updated: Jul 12, 2026

An Analog Macroscopic Technique for Studying Molecular Hydrodynamic Processes in Dense Gases and Liquids
11:03

An Analog Macroscopic Technique for Studying Molecular Hydrodynamic Processes in Dense Gases and Liquids

Published on: December 4, 2017

世界海洋の潮は,通常のモードから合成されたものです.

G W Platzman

    Science (New York, N.Y.)
    |May 6, 1983
    PubMed
    まとめ

    海洋の正常モードは,月面の潮を合成し,エネルギーモードはM(2) とK(1) の潮エネルギーを支配する. 海洋の潮反応の質 (Q) は摩擦制御の振動器に似ており,M(2) グローバルQは約10です.

    科学分野:

    • 海洋学 海洋学 海洋学
    • 地質物理学 地質物理学とは地質物理学です.
    • 潮のダイナミクス

    背景:

    • 潮強制は,海洋過程の重要な原動力である.
    • 潮モード内のエネルギー分布を理解することは,海洋学モデリングに不可欠です.

    研究 の 目的:

    • 海洋の通常のモードを使用して,M(2) とK(1) の潮を合成する.
    • 潮合成に異なるモードのエネルギー貢献を分析する.
    • 海洋の潮反応の質因子 (Q) を調査する.

    主な方法:

    • 潮合成のために60の海洋正常モードを利用した.
    • M 2) と K 1) の潮の最もエネルギーのあるモードの間のエネルギー分布を分析した.
    • 海洋反応の質 (Q) を決定するためにモデル計算を行った.

    主要な成果:

    • 最もエネルギーが消費される10のモードは,潮エネルギーの87%と,潮エネルギーの93%を占めた.
    • 29時間間の単一モードは,K(1) のエネルギーの3分の2を供給した.
    • モデル計算により,海洋の潮反応の質 (Q) は摩擦によって制御され,MのグローバルQは約10であることが明らかになった.

    さらに関連する動画

    Methods for Measuring the Orientation and Rotation Rate of 3D-printed Particles in Turbulence
    12:34

    Methods for Measuring the Orientation and Rotation Rate of 3D-printed Particles in Turbulence

    Published on: June 24, 2016

    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

    関連する実験動画

    Last Updated: Jul 12, 2026

    An Analog Macroscopic Technique for Studying Molecular Hydrodynamic Processes in Dense Gases and Liquids
    11:03

    An Analog Macroscopic Technique for Studying Molecular Hydrodynamic Processes in Dense Gases and Liquids

    Published on: December 4, 2017

    Methods for Measuring the Orientation and Rotation Rate of 3D-printed Particles in Turbulence
    12:34

    Methods for Measuring the Orientation and Rotation Rate of 3D-printed Particles in Turbulence

    Published on: June 24, 2016

    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

    結論:

    • 海洋の正常モードは,主要な潮成分を効果的に合成します.
    • いくつかのエネルギーモードが潮エネルギーを支配し,システムのダイナミクスを簡素化する.
    • 海洋の潮反応は,特定の品質因子によって特徴づけられる,減圧された振動器に似ています.