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相关概念视频

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...

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North atlantic ocean: preliminary description of normal modes.

Science (New York, N.Y.)·1972
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相关实验视频

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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

世界海洋潮由正常模式合成.

G W Platzman

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

    海洋的正常模式合成月球的潮,其中能量模式主导M(2) 和K(1) 潮能量. 海洋潮反应质量 (Q) 类似于摩擦控制的振荡器,M(2) 全球Q约为10.

    科学领域:

    • 海洋学 海洋学 海洋学
    • 地质物理学 地质物理学
    • 潮的动态 潮的动态

    背景情况:

    • 潮强迫是海洋过程的一个重要驱动因素.
    • 了解潮模式中的能量分布对于海洋学建模至关重要.

    研究的目的:

    • 使用海洋正常模式合成M(2) 和K(1) 潮.
    • 分析不同模式对潮合成的能量贡献.
    • 为了研究海洋潮反应的质量因子 (Q).

    主要方法:

    • 利用60个海洋正常模式进行潮合成.
    • 分析了M(2) 和K(1) 潮中最有能量模式之间的能量分布.
    • 执行模型计算以确定海洋响应质量 (Q).

    主要成果:

    • 十种能量最多的模式占M2) 潮能量的87%,K1) 潮能量的93%.
    • 一个29小时周期的单一模式贡献了三分之二的K(1) 能量.
    • 模型计算显示,海洋的潮反应质量 (Q) 是由摩擦控制的,M的全球Q约为10).

    结论:

    • 海洋正常模式有效地合成了主要的潮成分.

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  • 几种能量模式主导着潮能量,简化了系统的动态.
  • 海洋的潮反应类似于一个化振荡器,其特点是特定的质量因子.