Airglow

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Airglow is a faint emission of light by a planetary atmosphere. In the case of Earth's atmosphere, this optical phenomenon causes the night sky never to be completely dark, even after the effects of starlight and diffused sunlight from the far side are removed. This phenomenon originates with self-illuminated gases and has no relationship with Earth's magnetism or sunspot activity, causing .

Airglow occurs in two forms, resulting by two different processes, but both having the same cause. Airglow is caused by sunlight splitting atmospheric molecules, which at this point produce during day the dayglow called airglow, which is too faint to be seen in daylight. During the night airglow occurs as nightglow, resulting from the recombination of the molecules which were split during daytime.

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History The airglow phenomenon was first identified in 1868 by Swedish physicist Anders Ångström. Since then, it has been studied in the laboratory, and various chemical reactions have been observed to emit electromagnetic energy as part of the process. Scientists have identified some of those processes that would be present in Earth's atmosphere, and astronomers have verified that such emissions are present. Simon Newcomb was the first person to scientifically study and describe airglow, in 1901.M. G. J. Minnaert, De natuurkunde van 't vrije veld, Deel 2: Geluid, warmte, elektriciteit. § 248: Het ionosfeerlicht

Airglow was known to the ancient Greeks: "Aristotle and Pliny described the phenomena of Chasmata, which can be identified in part as auroras, and in part as bright airglow nights." Sciences of the Earth, An Encyclopedia of Events, People, and Phenomena, 1998, Garland Publishing, p. 35, via Google Books, access date 25 June 2022.

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Description Airglow looks similar to the at times stronger , though auroras are caused differently.

Airglow is caused by various processes in the upper atmosphere of Earth, such as the recombination of atoms which were photoionization by the Sun during the day, luminescence caused by striking the upper atmosphere, and chemiluminescence caused mainly by oxygen and nitrogen reacting with hydroxyl free radicals at heights of a few hundred kilometres. It is not noticeable during the daytime due to the glare and scattering of sunlight. The airglow resulting from the photoionization in daylight and the recombination at night is called dayglow and nightglow respectively.

Even at the best ground-based observatories, airglow limits the photosensitivity of optical telescopes. Partly for this reason, like Hubble can observe much fainter objects than current ground-based telescopes at visible spectrum.

Airglow at night may be bright enough for a ground observer to notice and appears generally bluish. Although airglow emission is fairly uniform across the atmosphere, it appears brightest at about 10° above the observer's horizon, since the lower one looks, the greater the mass of atmosphere one is looking through. Very low down, however, atmospheric extinction reduces the apparent brightness of the airglow.

One airglow mechanism is when an atom of nitrogen combines with an atom of oxygen to form a molecule of nitric oxide (NO). In the process, a photon is emitted. This photon may have any of several different wavelengths characteristic of nitric oxide molecules. The free atoms are available for this process, because molecules of nitrogen (N₂) and oxygen (O₂) are dissociated by solar energy in the upper reaches of the atmosphere and may encounter each other to form NO. Other chemicals that can create air glow in the atmosphere are hydroxyl (OH), atomic oxygen (O), sodium (Na), and lithium (Li).

The sky brightness is typically measured in units of apparent magnitude per square arcsecond of sky.

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Calculation In order to calculate the relative intensity of airglow, we need to convert apparent magnitudes into fluxes of photons; this clearly depends on the spectrum of the source, but we will ignore that initially. At visible wavelengths, we need the parameter S₀( V), the power per square centimetre of aperture and per micrometre of wavelength produced by a zeroth-magnitude star, to convert apparent magnitudes into fluxes – . High Energy Astrophysics: Particles, Photons and Their Detection Vol 1, Malcolm S. Longair, If we take the example of a star observed through a normal V band filter ( bandpass, frequency ), the number of photons we receive per square centimeter of telescope aperture per second from the source is N_s:

$N\_\backslash text\{s\}\; =\; 10^\{-28/2.5\}\backslash times\backslash frac\{S\_0(V)\; \backslash times\; B\}\{h\backslash nu\}$

(where h is the Planck constant; hν is the energy of a single photon of frequency ν).

At V band, the emission from airglow is per square arc-second at a high-altitude observatory on a moonless night; in excellent seeing conditions, the image of a star will be about 0.7 arc-second across with an area of 0.4 square arc-second, and so the emission from airglow over the area of the image corresponds to about . This gives the number of photons from airglow, N_a:

$N\_\backslash text\{a\}\; =\; 10^\{-23/2.5\}\backslash times\backslash frac\{S\_0(V)\; \backslash times\; B\}\{h\backslash nu\}$

The signal-to-noise for an ideal ground-based observation with a telescope of area A (ignoring losses and detector noise), arising from Poisson statistics, is only:

$S/N\; =\; \backslash sqrt\{A\}\backslash times\backslash frac\{N\_\backslash text\{s\}\}\{\backslash sqrt\{N\_\backslash text\{s\}+N\_\backslash text\{a\}\}\}$

If we assume a 10 m diameter ideal ground-based telescope and an unresolved star: every second, over a patch the size of the seeing-enlarged image of the star, 35 photons arrive from the star and 3500 from air-glow. So, over an hour, roughly arrive from the air-glow, and approximately arrive from the source; so the S/ N ratio is about:

$\backslash frac\{1.3\; \backslash times\; 10^5\}\{\backslash sqrt\{1.3\; \backslash times\; 10^7\}\}\; \backslash approx\; 36.$

We can compare this with "real" answers from exposure time calculators. For an 8 m unit Very Large Telescope telescope, according to the FORS exposure time calculator, 40 hours of observing time are needed to reach , while the 2.4 m Hubble only takes 4 hours according to the ACS exposure time calculator. A hypothetical 8 m Hubble telescope would take about 30 minutes.

This calculation shows that reducing the view field size can make fainter objects more detectable against the airglow; unfortunately, adaptive optics techniques that reduce the diameter of the view field of an Earth-based telescope by an order of magnitude only as yet work in the infrared, where the sky is much brighter. A space telescope is not restricted by the view field, since it is not affected by airglow.

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Induced airglow Scientific experiments have been conducted to induce airglow by directing high-power radio emissions at the Earth's ionosphere. HF-induced airglow at magnetic zenith: Thermal and parametric instabilities near electron gyroharmonics. E.V. Mishin et al., Geophysical Research Letters Vol. 32, L23106, , 2005 These radiowaves interact with the ionosphere to induce faint but visible optical light at specific wavelengths under certain conditions. NRL HAARP Overview . Naval Research Laboratory. The effect is also observable in the radio frequency band, using .

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Experimental observation SwissCube-1 is a Switzerland satellite operated by Ecole Polytechnique Fédérale de Lausanne. The spacecraft is a single unit CubeSat, which was designed to conduct research into airglow within the Earth's atmosphere and to develop technology for future spacecraft. Though SwissCube-1 is rather small (10 cm × 10 cm × 10 cm) and weighs less than 1 kg, it carries a small telescope for obtaining images of the airglow. The first SwissCube-1 image came down on 18 February 2011 and was quite black with some thermal noise on it. The first airglow image came down on 3 March 2011. This image has been converted to the human optical range (green) from its near-infrared measurement. This image provides a measurement of the intensity of the airglow phenomenon in the near-infrared. The range measured is from 500 to 61400 photons, with a resolution of 500 photons. SwissCube official website

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Observation of airglow on other planets The Venus Express spacecraft contains an infrared sensor which has detected near-IR emissions from the upper atmosphere of Venus. The emissions come from nitric oxide (NO) and from molecular oxygen. Scientists had previously determined in laboratory testing that during NO production, ultraviolet emissions and near-IR emissions were produced. The UV radiation had been detected in the atmosphere, but until this mission, the atmosphere-produced near-IR emissions were only theoretical.

Airglow on Venus is the most likely candidate for the illusive ashen light having been observed from Earth since the 17th century.

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Gallery Airglow over La Silla’s Great Dane.jpg|Hues of red and green lighting up the sky are produced by airglow. Airglow over Paranal Observatory, Chile.jpg|Airglow over Paranal Observatory. Panoramic shot of the VLT platform.jpg|Airglow over the VLT platform Airglow in France (01-21-2023).jpg|Airglow over Dordogne, France. Tumblr inline ph0ungGXF31tzhl5u 500-1.gif|Airglow timelapse from space, with a broad red band of airglow.

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See also

• Earthlight
• Ionized-air glow
• Optical phenomena
• Polar aurora
• Zodiacal light

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External links

• Description and Images
• Sky Brightness Information for Roque de los Muchachos Observatory
• Night-side Glow Detected at Mars Space.com interview
• Stereoscopic Observations of HAARP Glows from HIPAS, Poker Flat, and Nenana, Alaska by R.F. Wuerker et al.
• An improved signal-to-noise ratio of a cool imaging photon detector for Fabry - Perot interferometer measurements of low-intensity air glow by T P Davies and P L Dyson
• Space Telescope Imaging Spectrograph Instrument Handbook for Cycle 13
• SwissCube| The first Swiss Satellite

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