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Related Concept Videos

Photoelectric Effect02:26

Photoelectric Effect

When light of a particular wavelength strikes a metal surface, electrons are emitted. This is called the photoelectric effect. The minimum frequency of light that can cause such emission of electrons is called the threshold frequency, which is specific to the metal. Light with a frequency lower than the threshold frequency, even if it is of high intensity, cannot initiate the emission of electrons. However, when the frequency is higher than the threshold value, the number of electrons ejected...
Schwarzschild Radius and Event Horizon01:21

Schwarzschild Radius and Event Horizon

No object with a finite mass can travel faster than the speed of light in a vacuum. This fact has an interesting consequence in the domain of extremely high gravitational fields.
The minimum speed required to launch a projectile from the surface of an object to which it is gravitationally bound so that it eventually escapes the object’s gravitational field is called the escape velocity. The escape velocity is independent of the mass of the object. Merging the idea of escape velocity with the...
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Detection of Black Holes

Although black holes were theoretically postulated in the 1920s, they remained outside the domain of observational astronomy until the 1970s.
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Magnetic Declination01:19

Magnetic Declination

Magnetic declination is the angle between true north, which aligns with the Earth's rotational axis, and magnetic north, which follows the direction of the Earth's magnetic field. This discrepancy exists because the magnetic poles do not coincide with the geographic poles. The value of magnetic declination depends on the observer's location on Earth and is subject to changes over time due to the dynamic nature of the Earth's magnetic field.The declination is called eastern when magnetic north...
Group Polarization01:01

Group Polarization

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Related Experiment Video

Updated: Jun 16, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Sky brightness and polarization during the 1973 african eclipse.

G E Shaw

    Applied Optics
    |February 6, 2010
    PubMed
    Summary

    Sky color and polarization changed dramatically during a 1973 solar eclipse. Measurements showed decreased sky radiance and polarization, with spectral shifts toward blue at the zenith and red at the horizon.

    Area of Science:

    • Atmospheric optics
    • Solar eclipses
    • Radiative transfer

    Background:

    • Solar eclipses significantly alter atmospheric conditions.
    • Understanding sky radiance and polarization is crucial for atmospheric studies.

    Purpose of the Study:

    • To measure the absolute intensity, color, and polarization of the sky during the June 30, 1973, solar eclipse.
    • To analyze changes in zenith sky radiance, spectral distribution, and polarization ratio.

    Main Methods:

    • Absolute intensity, color, and polarization measurements of the sky.
    • Analysis of zenith sky radiance, spectral distribution, and polarization ratio.
    • Comparison of results with radiative transfer models.

    Main Results:

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    • Zenith sky radiance decreased by a factor of 10,000 during totality.
    • Sky spectral distribution shifted towards blue at the zenith and reddened at the horizon.
    • Polarization ratio decreased significantly from 0.45 to 0.04, influenced by surface albedo.

    Conclusions:

    • Observed sky changes during the eclipse are consistent with a double-scattering radiative transfer model.
    • Surface albedo plays a significant role in the distribution of sky polarization.