Atmospheric Distortion

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Many people believe that astronomers want to build telescopes on tall mountains or put them in space, so they can be ``closer'' to the objects they are observing. This is INcorrect! The nearest star is over 41,500,000,000,000 kilometers (26 trillion miles) away. If you ignore the 300-million kilometer variation in the distances due to the Earth's motion around the Sun and the 12,756-kilometer variation due to the Earth's rotation, being 4 kilometers closer on a tall mountain amounts to a difference of at most 1 × 10-11 percent. Telescopes in space get up to 1 × 10-9 percent closer (again ignoring the much larger variations of the Earth's orbit around the Sun and the telescope's orbit around the Earth). These are extremely small differences---the distances to the even the nearest stars are around 100,000's times greater than the distances between the planets in our solar system. The reason large telescopes are built on tall mountains or put in space is to get away from the distortion of starlight due to the atmosphere.

Kitt Peak National Observatory The famous observing site at the Kitt Peak National Observatory has many large telescopes including the 4-meter Mayall telescope (top right) and the McMath Solar Telescope (triangular one at the lower right). Although it is over 60 kilometers from Tucson, AZ, light pollution from the increasing population of that city has stopped the construction of any more telescopes on the mountain.

The Mauna Kea Observatory is probably the best observing site in the world. Many very large telescopes are at the 4177-meter summit of the extinct volcano. Because of the elevation, the telescopes are above most of the water vapor in the atmosphere, so infrared astronomy can be done. Kitt Peak's elevation of 2070 meters is too low for infrared telescopes.

Mauna Kea Observatory

The James C. Maxwell Telescope is in the center front of this picture of the Mauna Kea Observatory. The two white Keck 10-meter telescopes are to the left on the ridgetop next to the silver 8.3-meter Subaru telescope. Select the image to go to the Mauna Kea Observatory homepage.

Seeing

The air is constantly in turbulent motion and light from celestial objects is bent randomly in many ways over time periods of tens of milliseconds. Images dance about (twinkle) and images are blurred. The atmospheric blurring distorts the view of astronomical objects much as ripples in water distort the objects below the surface. This atmospheric effect is called seeing.

turbulent 
air makes poor seeing

The short animation shows how light from a star is refracted in random directions by rapidly-moving pockets of air of varying densities and temperatures. The light reaches different parts of the telescope's objective from slightly different directions and different times. A highly magnified view shows multiple images of the star that dance about in the field of view many times a second, so a second or longer exposure picture will show a fuzzy blob (called the ``seeing disk'') the size of the entire distribution of dancing images. An actual observation shows much more rapid variation and more images of the star. A movie (mpeg format) of a binary star is available by selecting this link. The data is from the William Herschel 4.2-meter Telescope in La Palma, Chile and is courtesy of the Applied Optics Group at Imperial College. Links to other movies are available there.

Good seeing is when the air is stable (little turbulence) and the twinkling is small. Details as small as 0.5 arc seconds can be seen when the seeing is good (still much larger than the theoretical resolving power of large research telescopes). Poor seeing happens when the air is turbulent so the images dance about and details smaller than 2 to 3 arc seconds cannot be seen. The more atmosphere there is above a telescope, the greater is the turbulent motion and the poorer is the seeing. This is one reason why research telescopes are located on very high mountains.

less 
atmosphere makes better seeing

Speckle interferometry can get rid of atmospheric distortion by taking many fast exposures of an object. Each fraction-of-a-second exposure freezes the motion of the object. Extensive computer processing then shifts the images to a common center and removes other noise and distortions caused by the atmosphere, telescope, and electronics to build up a distortion-free image. See Chris Koresko's thesis for further exploration of speckle interferometry. Another technique called adaptive optics makes quick changes in the light path of the optics to compensate for the atmospheric turbulence. Before the focussed light from the objective reaches the camera, it bounces off a thin deformable mirror that can be adjusted thousands of times a second to reposition the multiple images back to the center. An excellent site to explore this topic further is the Center for Astronomical Adaptive Optics web site. A comparison of speckle interferometry and adaptive optics is at Koresko's Starfire infrared imaging site.

Hubble Space 
Telescope

Telescopes in orbit like the Hubble Space Telescope are above the turbulent effect of the atmosphere and can achieve their theoretical resolving power. The Hubble Space Telescope has a 2.4-meter objective, making it the largest telescope ever put in orbit. One major drawback to satellite observatories is the large cost to build and maintain them. Advances in adaptive optics may soon remove the seeing effects and enable the huge research telescopes to take even sharper pictures than those from the Hubble Space Telescope.

Reddening and Extinction

The air also absorbs and scatters electromagnetic radiation by an amount that varies with the wavelength. Redder (longer wavelength) light is scattered less by atmosphere molecules and dust than bluer (shorter wavelength) light. This effect is known as reddening. This effect explains why the Sun appears orange or red when it is close to the horizon. The other colors of sunlight are scattered out of your line of sight so that only the orange and red colors make it through the atmosphere to your eyes. This effect also explains why the sky is blue. Since blue light is scattered more, you will see more blue light scattered back to your eyes when you look in a direction away from the Sun.

why the 
sky is blue and sunsets are orange-red

All wavelengths of light are scattered or absorbed by some amount. This effect is called extinction. Some wavelength bands suffer more extinction than others. Some of the infrared band can be observed from mountains above 2750 meters elevation, because the telescopes are above most of the water vapor in the air. Carbon dioxide also absorbs a lesser amount of the infrared energy. Gamma-rays and X-rays are absorbed by oxygen and nitrogen molecules very high above the surface, so none of this very short wavelength radiation makes it to within 100 kilometers of the surface. The ultraviolet light is absorbed by the oxygen and ozone molecules at altitudes of about 60 kilometers. The longest wavelengths of the radio band are blocked by electrons at altitudes around 200 kilometers.

The Hubble Space Telescope (HST) is able to observe in the ultraviolet, something that ground-based research telescopes cannot do. This is one advantage that HST will always have over ground-based telescopes, even those with adaptive optics. Even though HST has a smaller objective than many ground-based telescopes, its ability to observe in shorter wavelengths will keep its resolving power very competitive with the largest ground-based telescopes with the best adaptive optics.

Telescopes used to observe in the high-energy end of the electromagnetic spectrum must be put above the atmosphere and require special arrangements of their reflecting surfaces. The extreme ultraviolet and X-rays cannot be focussed using an ordinary mirror because the high-energy photons would bury themselves into the mirror. But if they hit the reflecting surface at a very shallow angle, they will bounce off. Using series of concentric cone-shaped metal plates, high energy ultraviolet and X-ray photons can be focussed to make an image.

grazing incidence mirrors for high-energy photons

Gamma rays have too high an energy to be focussed with even the shallow angle reflecting technique, so gamma ray telescopes simply point in a desired direction and count the number of photons coming from that direction. Some examples of high-energy space observatories are shown below. Clicking on the images will take you to sites describing the telescopes in greater detail. The first picture is of the Extreme Ultraviolet Explorer spacecraft that observes in the short-wavelength end of the ultraviolet band. The Roentgen Satellite (ROSAT) is in the second picture. It observes in the X-ray band. The third picture shows a telescope that observes the most energetic forms of electromagnetic radiation---gamma rays. It is called the Compton Gamma Ray Observatory.

EUVE spacecraft
The Extreme Ultraviolet Explorer

ROSAT spacecraft
The Roentgen Satellite (ROSAT)

Compton GRO
The Compton Gamma Ray Observatory

Atmospheric lines

Gases in the Earth's atmosphere can introduce extra absorption lines into the spectra of celestial objects. The atmospheric spectral lines must be removed from the spectroscopy data, otherwise astronomers will find a hot star with molecular nitrogen, oxygen and water lines! Such lines are only produced by gases much cooler than that in stars.

Vocabulary

adaptive optics extinction reddening
seeing speckle interferometry

Review Questions

  1. The distance to the nearest star is 4.3 light years = 4.3 × 9.7 trillion kilometers = 41,800,000,000,000 km. Does Mauna Kea's elevation of 4177 meters (=2.6 miles) put it significantly closer to even the nearest star than something at sea level? Explain your answer. (1 kilometer = 1000 meters.)
  2. What causes stars to twinkle? What would make good seeing?
  3. Even with perfectly clear skies free of human-made pollution, the seeing on Mauna Kea (4177 meters elevation) is much better than at sea level. Why is that?
  4. What absorbs infrared light in our atmosphere and up to what height above sea level is most of this IR absorber found?
  5. Even with perfectly clear skies free of human-made pollution, infrared observations can be made at Mauna Kea but not at Kitt Peak (2070 meters elevation). Why is that?
  6. Why are all ultraviolet, X-ray, and gamma ray telescopes put up in orbit?

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last updated 20 October 1999


Is this page a copy of Strobel's Astronomy Notes?
Author of original content: Nick Strobel