Twinkling
Twinkling is atmospheric scintillation affecting distant light sources.
Twinkling, also called scintillation, is a generic term for variations in apparent brightness, colour, or position of a distant luminous object viewed through a medium. It is a key factor in astronomical seeing, alongside light pollution and cloud cover, and is caused by light passing through turbulent layers of Earth's atmosphere.
- field
- Atmospheric optics, observational astronomy
- known_for
- Variations in apparent brightness, colour, or position of distant luminous objects due to atmospheric refraction
- types
- Astronomical scintillation (objects outside atmosphere) and terrestrial scintillation (objects within atmosphere)
- measurement
- Scintillometer
Lore & Background
Twinkling, or scintillation, is a generic term for variations in apparent brightness, colour, or position of a distant luminous object viewed through a medium. When the object lies outside Earth's atmosphere, as with stars and planets, the phenomenon is termed astronomical scintillation; for objects within the atmosphere, it is terrestrial scintillation. Atmospheric scintillation is defined as variations in illuminance only, and it is one of the three principal factors governing astronomical seeing, the others being light pollution and cloud cover.
Reader's Guide
Twinkling is caused by the passing of light through different layers of a turbulent atmosphere, with most effects due to anomalous atmospheric refraction from small-scale fluctuations in air density, usually related to temperature gradients. Scintillation effects are always much more pronounced near the horizon than near the zenith, because light rays near the horizon travel longer paths through the atmosphere. The effects of twinkling are reduced by using a larger receiver aperture, an effect known as aperture averaging, and many modern large telescopes use adaptive optical systems that precisely deform a mirror's figure to compensate for scintillation. Stars twinkle because they appear as point sources of light easily disturbed by atmospheric turbulence, while planets and the Moon, having observable diameters, show less variation as their multiple light points average out deviations.
Did You Know?
- Twinkling is also called scintillation.
- Atmospheric scintillation is defined as variations in illuminance only.
- Scintillation effects are much more pronounced near the horizon than near the zenith.
- Using a larger receiver aperture reduces twinkling effects, a phenomenon known as aperture averaging.
Frequently Asked Questions
What is Twinkling in astronomical terms?
Twinkling, formally called scintillation, describes the fluctuating brightness, colour, or apparent position of a distant light source as seen through an intervening medium. It sits at the intersection of atmospheric optics and observational astronomy.
What causes Twinkling?
The effect arises when light from a distant source passes through turbulent layers of Earth's atmosphere, which refract the photons unevenly. The ever-shifting air currents bend the light in slightly different directions moment to moment, producing the familiar flicker.
How does Twinkling affect astronomical seeing?
Alongside light pollution and cloud cover, scintillation is a primary factor that limits an observer's seeing quality. It smears and dims point-like sources such as stars, making fine-detail work more difficult.
What are the two main types of Twinkling?
Astronomical scintillation refers to the effect on luminous objects located outside Earth's atmosphere, whereas terrestrial scintillation applies to objects situated within it. Both share the same underlying mechanism of turbulent atmospheric refraction.
What instrument is used to measure Twinkling?
A scintillometer is the dedicated device for quantifying the level of scintillation at a given observing site. Astronomers use its readings to characterise local atmospheric turbulence before planning sensitive photometric or astrometric observations.
More in Astronomical Concepts And Techniques 1-22
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