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関連する概念動画

Oscillations about an Equilibrium Position01:04

Oscillations about an Equilibrium Position

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Stability is an important concept in oscillation. If an equilibrium point is stable, a slight disturbance of an object that is initially at the stable equilibrium point will cause the object to oscillate around that point. For an unstable equilibrium point, if the object is disturbed slightly, it will not return to the equilibrium point. There are three conditions for equilibrium points—stable, unstable, and half-stable. A half-stable equilibrium point is also unstable, but is named so...
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Damped Oscillations01:07

Damped Oscillations

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In the real world, oscillations seldom follow true simple harmonic motion. A system that continues its motion indefinitely without losing its amplitude is termed undamped. However, friction of some sort usually dampens the motion, so it fades away or needs more force to continue. For example, a guitar string stops oscillating a few seconds after being plucked. Similarly, one must continually push a swing to keep a child swinging on a playground.
Although friction and other non-conservative...
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Types of Damping01:20

Types of Damping

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If the amount of damping in a system is gradually increased, the period and frequency start to become affected because damping opposes, and hence slows, the back and forth motion (the net force is smaller in both directions). If there is a very large amount of damping, the system does not even oscillate; instead, it slowly moves toward equilibrium. In brief, an overdamped system moves slowly towards equilibrium, whereas an underdamped system moves quickly to equilibrium but will oscillate about...
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Forced Oscillations01:06

Forced Oscillations

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When an oscillator is forced with a periodic driving force, the motion may seem chaotic. The motions of such oscillators are known as transients. After the transients die out, the oscillator reaches a steady state, where the motion is periodic, and the displacement is determined.
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Coriolis Force01:23

Coriolis Force

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An accelerating particle experiences a force equal to the mass multiplied by the acceleration in an inertial frame of reference. Consider a particle in a non-inertial frame of reference, such as a sliding ball on a rotating table. The acceleration of the ball in this rotating reference frame is different than in the intertial frame, which modifies its equation of motion. The fictitious forces acting additionally on a rotating frame of reference alter Newton's Second Law expression.
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Magnetostatic Boundary Conditions01:28

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An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
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Updated: Mar 31, 2026

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
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大西洋の多年周期振動は,海洋循環の役割なし

Amy Clement1, Katinka Bellomo2, Lisa N Murphy2

  • 1Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL, USA. aclement@rsmas.miami.edu.

Science (New York, N.Y.)
|October 17, 2015
PubMed
まとめ

大西洋多年周期振動 (AMO) は大気循環によって引き起こされ,大西洋南回転循環 (AMOC) のような海流によって引き起こされない. 気候モデルでは,海洋熱輸送が固定されている場合でも,この主要な気候変動モードの新たな理解を示唆しています.

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科学分野:

  • 気候科学
  • 海洋学
  • 大気科学

背景:

  • 大西洋多年周期振動 (AMO) は,社会に影響を与える重要な気候パターンです.
  • 主流の理論では,AMOの原動力は海洋循環,特に大西洋南側転覆循環 (AMOC) に起因すると考えられている.

研究 の 目的:

  • 大西洋多年周期振動 (AMO) の主要な要因を調査する.
  • AMOCがAMOの原因であるという確立された見解に異議を唱える.

主な方法:

  • 大気の影響を隔離するために,規定された海洋熱輸送を伴う気候モデルを使用した.
  • 海洋と大気の相互作用が AMOの特徴に与える影響を評価した.

主要な成果:

  • 気候モデルは,固定された海洋熱輸送で,重要なAMO特性を成功裏に再現しました.
  • インタラクティブな海洋-大気結合は,現在のモデルで AMOの特性を実質的に変更しませんでした.

結論:

  • AMOは中緯度の大気循環による ストキャスティック・フォースメントへの反応であるようです
  • AMOCのシフトを含む海洋循環の変化は,AMOの原因ではなく,結果である可能性が高い.
  • 熱帯の熱結合は AMO現象に 役割を果たしています