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Airglow over the VLT platform.[1]
A time-lapse taken on Cerro Paranal of the VLT. Faint airglow lingers on the horizon, and the Moon rises brilliantly at the end of the clip.

Airglow (also called nightglow) 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.

Airglow in the Central of France on 13th of August 2015


  • Development 1
  • Description 2
  • Calculation of the effects of airglow 3
  • Induced airglow 4
  • Experimental observation 5
  • Observation of airglow on other Solar System planets 6
  • See also 7
  • References 8
  • External links 9


The airglow phenomenon was first identified in 1868 by Swedish scientist 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.


Comet Lovejoy passing behind Earth's airglow on December 22, 2011

Airglow is caused by various processes in the upper atmosphere, such as the recombination of atoms which were photoionized by the sun during the day, luminescence caused by cosmic rays striking the upper atmosphere, and chemiluminescence caused mainly by oxygen and nitrogen reacting with hydroxyl ions at heights of a few hundred kilometres. It is not noticeable during the daytime because of the scattered light from the sun.

The airglow above the horizon, captured from the ISS

Even at the best ground-based observatories, airglow limits the sensitivity of telescopes at visible wavelengths. Partly for this reason, space-based telescopes such as the Hubble Space Telescope can observe much fainter objects than current ground-based telescopes at visible wavelengths.

The airglow at night may be bright enough to be noticed by an observer and is generally bluish in colour. Although airglow emission is fairly uniform across the atmosphere, to an observer on the ground it appears brightest at about 10 degrees above the horizon, because the lower one looks, the greater the depth 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 species that can create air glow in the atmosphere are hydroxyl (OH),[2][3][4] atomic oxygen (O), sodium (Na) and lithium (Li).[5] See Sodium layer.

The sky brightness is typically quoted in units of astronomical magnitudes per square arcsecond of sky.

Calculation of the effects of airglow

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 -- S_{0}(V)=4.0\times 10^{-12} W cm−2 µm−1.[6] If we take the example of a V=28 star observed through a normal V band filter (B=0.2 µm bandpass, frequency \nu \sim 6\times10^{14} Hz), the number of photons we receive per square centimeter of telescope aperture per second from the source is N_{s}:

N_{s}=10^{-28/2.5}\times\frac{S_{0}(V) \times B}{h\nu}

(where h is Planck's constant; h \nu is the energy of a single photon of frequency \nu).

At V band, the emission from airglow is V=22 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 V=23. This gives the number of photons from airglow, N_{a}:

N_{a}=10^{-23/2.5}\times\frac{S_{0}(V) \times B}{h\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 = \sqrt{A}\times\frac{N_{s}}{\sqrt{N_{s}+N_{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 1.3\times 10^7 \pm 3500 photons arrive from the air-glow, and approximately 1.3 \times 10^5 arrive from the source; so the S/N ratio is about : \frac{1.3 \times 10^5}{\sqrt{1.3 \times 10^7}} = 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 you need 40 hours of observing time to reach V = 28, 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.

It should be clear from this calculation 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 isn't restricted by the view field, since they are not impacted by airglow.

Induced airglow

Two images of the sky over the HAARP Gakona facility using the NRL-cooled CCD imager at 557.7 nm. The field of view is approximately 38°. The left-hand image shows the background star field with the HF transmitter off. The right-hand image was taken 63 seconds later with the HF transmitter on. Structure is evident in the emission region.

Scientific experiments have been conducted to induce airglow by directing high-power radio emissions at the Earth's ionosphere.[7] These radiowaves interact with the ionosphere to induce faint but visible optical light at specific wavelengths under certain conditions.[8]

Experimental observation

SwissCube-1's first airglow image of the Earth (shifted to green from near IR) captured on March 3, 2011.

SwissCube-1 is a Swiss 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 x 10 x 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 February 18, 2011 and was quite black with some thermal noise on it. The first airglow image came down on March 3, 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.[9]

Observation of airglow on other Solar System 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.[10] Scientists had previously determined in laboratory testing that during NO production, ultraviolet emissions and near-IR emissions were produced. The UV radiation has been detected in the atmosphere, but until this mission, the atmosphere-produced near-IR emissions were only theoretical.[11]

See also


  1. ^ "Austrian Software Tools Developed for ESO". European Southern Observatory. Retrieved 6 June 2014. 
  2. ^ A. B. Meinel (1950). "OH Emission Bands in the Spectrum of the Night Sky I.". Astrophysical Journal 111: 555.  
  3. ^ A. B. Meinel (1950). "OH Emission Bands in the Spectrum of the Night Sky II.". Astrophysical Journal 112: 120.  
  4. ^ F. W. High; et al. (2010). "Sky Variability in the y Band at the LSST Site". The Publications of the Astronomical Society of the Pacific 122 (892): 722–730.  
  5. ^ Origin of Sodium and Lithium in the Upper Atmosphere
  6. ^ High Energy Astrophysics: Particles, Photons and Their Detection Vol 1, Malcolm S. Longair, ISBN 0-521-38773-6
  7. ^ HF-induced airglow at magnetic zenith: Thermal and parametric instabilities near electron gyroharmonics. E.V. Mishin et al., Geophysical Research Letters Vol. 32, L23106, doi:10.1029/2005GL023864, 2005
  8. ^ NRL HAARP Overview. Naval Research Laboratory.
  9. ^ SwissCube official website
  10. ^ Garcia Munoz, A.; Mills, F. P.; Piccioni, G.; Drossart, P. (2009). "The near-infrared nitric oxide nightglow in the upper atmosphere of Venus". Proceedings of the National Academy of Sciences 106 (4): 985–988.  
  11. ^ Wilson, Elizabeth (2009). "PLANETARY SCIENCE Spectral band in Venus’ ‘nightglow’ allows study of NO, O". Chemical & Engineering News 87 (4): 11.  

External links

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