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Related Concept Videos

Apparent Weight and the Earth's Rotation01:28

Apparent Weight and the Earth's Rotation

Since all objects on the Earth's surface move through a circle every 24 hours, there must be a net centripetal force on each object, directed towards the center of that circle. The points of the north and south poles are the only exception to this rule.
For an object on the Earth's equator, the net centripetal force that accounts for its rotation is the Earth's pull towards its center, or the weight minus the normal force that prevents it from piercing into the Earth's surface. This force,...
Gyroscope: Precession01:24

Gyroscope: Precession

Precession can be demonstrated effectively through a spinning top. If a spinning top is placed on a flat surface near the surface of the Earth at a vertical angle and is not spinning, it will fall over due to the force of gravity producing a torque acting on its center of mass. However, if the top is spinning on its axis, it precesses about the vertical direction, rather than topple over due to this torque. Precessional motion is a combination of a steady circular motion of the axis and the...
Relative Motion Analysis using Rotating Axes01:25

Relative Motion Analysis using Rotating Axes

Consider a component AB undergoing a linear motion. Along with a linear motion, point B also rotates around point A. To comprehend this complex movement, position vectors for both points A and B are established using a stationary reference frame.
However, to express the relative position of point B relative to point A, an additional frame of reference, denoted as x'y', is necessary. This additional frame not only translates but also rotates relative to the fixed frame, making it instrumental in...
Rotational Motion about a Fixed Axis01:26

Rotational Motion about a Fixed Axis

A rigid body's rotation around a fixed axis makes every point within it trace a circular path around a specific line or point. The term given to this type of spinning is defined by the angular position, symbolized by the angle θ. This angle is gauged from a static reference line to the revolving object. From this angular position, any variation is referred to as angular displacement, denoted by dθ. The extent of this displacement can be calculated in degrees, radians, or revolutions, where one...
Kinematic Equations for Rotation01:30

Kinematic Equations for Rotation

In mechanics, when one observes a rigid body in rotational motion with constant angular acceleration, it is possible to establish equations for its rotational kinematics. This process resembles how linear kinematics are dealt with in simpler motion studies.
For instance, imagine a point A on a rigid body engaged in circular motion. The translational velocity of this particular point can be calculated by taking the time derivatives of the displacement equation, which essentially measures the...
Relative Motion Analysis using Rotating Axes - Acceleration01:22

Relative Motion Analysis using Rotating Axes - Acceleration

Consider a component AB undergoing a linear motion. Along with a linear motion, point B also rotates around point A. To comprehend this complex movement, position vectors for both points A and B are established using a stationary reference frame. The absolute velocity of point B is determined by adding the absolute velocity of point A, the relative velocity of point B in the rotating frame, and the effects caused by the angular velocity within the rotating frame.
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Methods for Measuring the Orientation and Rotation Rate of 3D-printed Particles in Turbulence
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Observations of Time Variation in the Sun's Rotation.

M F Woodard, K G Libbrecht

    Science (New York, N.Y.)
    |June 18, 1993
    PubMed
    Summary

    Solar cycle variations cause small changes in the Sun's subsurface rotation. These angular velocity shifts, primarily at high latitudes, are linked to solar activity.

    Area of Science:

    • * Solar Physics
    • * Helioseismology
    • * Solar Dynamo

    Background:

    • * Solar p-mode frequency splittings provide insights into the Sun's internal structure and dynamics.
    • * Previous helioseismic observations indicated solar cycle-related variations in the Sun's interior.

    Purpose of the Study:

    • * To investigate changes in the Sun's subsurface angular velocity over a solar cycle using helioseismic data.
    • * To determine the latitude dependence of solar rotation rate variations.
    • * To explore potential links between observed angular velocity changes and solar activity.

    Main Methods:

    • * Analysis of solar p-mode frequency splitting data from Big Bear Solar Observatory (1986 and 1988-90).
    • * Application of asymptotic inversion techniques to helioseismic data.

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  • * Comparison of rotation rates at different solar latitudes and time periods.
  • Main Results:

    • * Small (approx. 1%) changes in subsurface angular velocity were detected correlating with the solar cycle.
    • * The largest angular velocity variations (approx. 4 nHz) occurred between 1986 and 1988-90 at high solar latitudes (approx. 60 degrees).
    • * Helioseismology revealed latitude-dependent rotation rate changes.

    Conclusions:

    • * The Sun's subsurface rotation rate varies with the solar cycle, particularly at high latitudes.
    • * Observed angular velocity changes are consistent in magnitude with earlier suggestions regarding solar cycle influences on the solar convection zone.
    • * A detailed model explaining these solar cycle-induced angular velocity variations is still needed.