Extinction (astronomy)

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Extinction is a term used in astronomy to describe the absorption and scattering of light emitted by astronomical objects by matter (dust and gas) between the emitting object and the observer. For Earth-bound observers, extinction arises both from the interstellar medium (ISM) and the Earth's atmosphere; it may also arise from circumstellar dust around an observed object. The strong atmospheric extinction in some wavelength regions (for example X-ray, ultraviolet, and infrared) requires the use of Space-based observatories. Since blue light is much more strongly attenuated than red light in the optical wavelength regions, resulting in an object which is redder than expected, interstellar extinction is often termed reddening.

[edit] General Characteristics

Broadly speaking, interstellar extinction varies with wavelength such that the shorter the wavelength the stronger the extinction. Superimposed on this general trend are absorption features, which have various origins and can give clues as to the composition of dust grains. Known discrete absorptions features include (but not limited to) the 2175 Å bump, the diffuse interstellar bands, the 3.1 μm water ice feature, and the 10 and 18 μm silicate features.

The general shape of the ultraviolet through near-infared (0.125 to 3.5 μm) extinction curve in our own Galaxy, the Milky Way, is fairly well characterized by the single parameter R(V),^[1][2] but there are known deviations from this single parameter characterization.^[3] The R(V) parameter equals A(V)/E(B-V) and is a measurement of the total, A(V), to selective, E(B-V) = A(B)-A(V), extinction. R(V) is known to be correlated with the average dust grain size. For our own Galaxy, the Milky Way, the typical value for R(V) is 3.1.^[4] The relationship between the total extinction, A(V), and the amount of hydrogen, N_H = number of hydrogen atoms in a 1 cm² column, gives how the gas and dust in the interstellar medium are related. From studies using ultraviolet spectroscopy of reddened stars and X-ray scattering halos in the Milky Way, the relationship

has been determined.^[5][6][7]

[edit] Measuring extinction towards an object

To measure the extinction curve for a star, the star's spectrum is compared to the observed spectrum of a similar star known not to be affected by extinction (unreddened).^[8] It is also possible to use a theoretical spectrum instead of the observed spectrum for the comparison, but this is less common. In the case of emission nebulae, it is common to look at the ratio of two emission lines which should not be affected by the temperature and density in the nebula. For example, the ratio of hydrogen alpha to hydrogen beta emission is always around 2.85 under a wide range of conditions prevailing in nebulae. A ratio other than 2.85 must therefore be due to extinction, and the amount of extinction can thus be calculated.

[edit] The 2175 Å feature

One prominent feature in measured extinction curves of many objects within the Milky Way is a broad 'bump' at about 2175 Å, well into the ultraviolet region of the electromagnetic spectrum. This feature was first observed in the 1960s^[9][10] but its origin is still not well understood. Several models have been presented to account for this bump which include graphitic grains with a mixture of PAH molecules. Investigations of interstellar grains embedded in interplanetary dust particles (IDP) observed this feature and identified the carrier with organic carbon and amorphous silicates present in the grains.^[11]

[edit] Extinction curves of other galaxies

Plot showing the average extinction curves for the MW, LMC2, LMC, and SMC Bar.^[12] The curves are plotted versus 1/wavelength to emphasize the UV.

The form of the standard extinction curve depends on the composition of the ISM, which varies from galaxy to galaxy. In the Local Group, the best-determined extinction curves are those of the Milky Way, the Small Magellanic Cloud (SMC) and the Large Magellanic Cloud (LMC). In the LMC, there is significant variation in the characertistics of the ultraviolet extinction with a weaker 2175 Å bump and stronger far-UV extinction in the region associated with the LMC2 supershell (near the 30 Doradus starbursting region) than seen elsewhere in the LMC and in the Milky Way.^[13][14] In the SMC, more extreme variation is seen with no 2175 Å and very strong far-UV extinction in the star forming Bar and fairly normal ultraviolet extinction seen in the more quiescent Wing.^[15][16][17] This gives clues as to the composition of the ISM in the various galaxies. Previously, the different average extinction curves in the Milky Way, LMC, and SMC were thought to be the result of the different metallicities of the three galaxies: the LMC's metallicity is about 40% of that of the Milky Way, while the SMC's is about 10%. Finding extinction curves in both the LMC and SMC which are similar to those found in the Milky Way^[12] and finding extinction curves in the Milky Way that look more like those found in the LMC2 supershell of the LMC^[18] and in the SMC Bar^[19] has given rise to a new interpretation. The variations in the curves seen in the Magellanic Clouds and Milky Way may instead be caused by processing of the dust grains by nearby star formation. This interpretation is supported by work in starburst galaxies (which are undergoing intense star formation episodes) that their dust lacks the 2175 Å bump.^[20][21]

[edit] Atmospheric extinction

Atmospheric extinction varies with location and altitude. Astronomical observatories generally are able to characterise the local extinction curve very accurately, to allow observations to be corrected for the effect. Nevertheless, the atmosphere is completely opaque to many wavelengths requiring the use of satellites to make observations.

Atmospheric extinction has three main components: Rayleigh scattering by air molecules, scattering by aerosols, and molecular absorption. Molecular absorption is often referred to as 'telluric absorption', as it is caused by the Earth ("telluric" is a synonym of "terrestrial"). The most important sources of telluric absorption are molecular oxygen and ozone, which absorb strongly in the near-ultraviolet, and water, which absorbs strongly in the infrared.

The amount of atmospheric extinction depends on the altitude of an object, being lowest at the zenith and at a maximum near the horizon. It is calculated by multiplying the standard atmospheric extinction curve by the mean airmass calculated over the duration of the observation.

[edit] References

[edit] General References for Article

1. Binney, J. and Merrifield, M., 1998, Galactic Astronomy, Princeton University Press
2. Howarth I.D. (1983), LMC and galactic extinction, Royal Astronomical Society, Monthly Notices, vol. 203, Apr. 1983, p. 301-304.
3. King D.L. (1985), Atmospheric Extinction at the Roque de los Muchachos Observatory, La Palma, RGO/La Palma technical note 31
4. Rouleau F., Henning T., Stognienko R. (1997), Constraints on the properties of the 2175Å interstellar feature carrier, Astronomy and Astrophysics, v.322, p.633-645