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orbiting observatory

 
 
Columbia Encyclopedia: orbiting observatory
observatory, orbiting, research satellite designed to study solar radiation, electromagnetic radiation from distant stars, the earth's atmosphere, or the like. Because the atmosphere and other aspects of the earth's environment interfere with astronomical observations from the ground, especially in the ultraviolet and infrared portions of the spectrum, the decades since the 1960s have seen increasing emphasis on space-based observatories.

The U.S. Orbiting Solar Observatory (OSO) program, comprising eight satellites launched between 1962 and 1971, was one of the earliest series of orbiting observatories; it studied the sun's atmosphere and the sunspot cycle. Also beginning in 1962 and extending through 1979 were the launches of the six satellites in Great Britain's Ariel program, which concentrated on solar ultraviolet and X radiation. The Orbiting Geophysical Observatory (OGO) program consisted of six satellites, launched between 1964 and 1969, that provided data on the earth's atmosphere, ionosphere, and magnetosphere and on the solar wind. The Orbiting Astronomical Observatory (OAO) program comprised four satellites, launched between 1966 and 1972, that studied astronomical phenomena at ultraviolet and X-ray wavelengths inaccessible to earthbound equipment.

In the following years, a large number of satellites were launched to study solar and galactic radio waves, X rays, gamma rays, and ultraviolet rays. In addition to the United States a number of countries participated, among them the Netherlands with ANS-1 (1974-76), which studied soft and hard X radiation; India with Aryabhata (1975), which returned atmospheric data for only four days before being silenced by a power failure; Japan with Hakucho (1979-85) and Tenma (1981-84), both of which studied X radiation; and the European Space Agency (ESA) with Exosat (1983-86), an X-ray observatory. This period also saw the first cooperative efforts, such as the International Ultraviolet Explorer (IUE), a joint effort of the United States, ESA, and Great Britain (1978-96), which returned data on ultraviolet radiation for 18 years.

ROSAT [Roentgen Satellite] (1990-99), a joint German-U.S.-British project, studied both X-ray and ultraviolet wavelengths never before imaged from space. It detected a new class of bright stars that shine only in the ultraviolet part of the spectrum and X-ray emissions from comets. The Cosmic Background Explorer (1989-93) studied microwave background radiation that no star or other known object could emit-it is believed to have come from the creation of the universe (see cosmology). The Infrared Space Observatory (ISO; 1995-98), launched by ESA, found water in the Orion nebula and in the atmospheres of the giant planets and Titan, found fluoride molecules in interstellar space, and studied the "cool" galaxies first seen by the Infrared Astronomy Satellite (IRAS) in 1983. Another European-built orbiting observatory, the Solar and Heliospheric Observatory (SOHO), was launched by NASA in 1995. After reaching a position about 950,000 mi (1.5 million km) from the earth, where the gravitational attraction of the earth and the sun are in balance (called a Lagrangian point), SOHO initiated a program of solar physics studies, such as the solar wind and solar plumes.

To fully explore the cosmos it is necessary to collect and analyze radiation emitted by phenomena throughout the entire electromagnetic spectrum. Toward that end, NASA proposed the concept of great observatories, a series of four orbiting observatories designed to conduct astronomical studies over many different wavelengths. An important aspect of the program was to overlap the operations phases of the missions to enable astronomers to make concurrent observations of an object at different spectral wavelengths. The first member of the program and the largest orbiting observatory is the Hubble Space Telescope (HST), which was deployed by a space shuttle in 1990 and repaired in orbit in 1993. Subsequent servicing missions added capabilities to the HST, which observes the universe at ultraviolet, visual, and near-infrared wavelengths. The second great observatory, the Compton Gamma-Ray Observatory, was launched and deployed by a shuttle in 1991; it collected data on gamma-ray bursts, which are some of the most violent physical processes in the universe. The third great observatory, the Chandra X-ray Observatory, formerly called the Advanced X-ray Astrophysics Facility, was deployed from a shuttle and boosted into a high earth orbit in 1999; it focuses on such objects as black holes, quasars, and high-temperature gases throughout the X-ray portion of the electromagnetic spectrum. The Spitzer Space Telescope, formerly the Space Infrared Telescope Facility, represents the fourth and final element in the great observatory program; launched in Aug., 2003, it fills an important gap in wavelength coverage not available from earthbound telescopes.

See also gamma-ray astronomy; infrared astronomy; space probe; ultraviolet astronomy; X-ray astronomy.


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Wikipedia: Space observatory
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Space observatories
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Space observatories and their wavelength working ranges
Website http://nssdc.gsfc.nasa.gov/astro/astrolist.html
Space Observatories and their wavelength working range. Inspired by http://www.spitzer.caltech.edu/Media/mediaimages/background.shtml
Spitzer, Hubble and XMM with their most important parts depicted

A space observatory is any instrument in outer space which is used for observation of distant planets, galaxies, and other outer space objects. This category is distinct from other observatories located in space that are pointed toward the earth for the purpose of reconnaissance and other types of information gathering.

Introduction

A large number of observatories have been launched into orbit, and most of them have greatly enhanced our knowledge of the Cosmos.

Performing astronomy from the Earth's surface is limited by the filtering and distortion of electromagnetic radiation (scintillation or twinkling) due to the Earth's atmosphere. Some terrestrial telescopes (such as the Very Large Telescope) can reduce atmospheric effects with adaptive optics. A telescope orbiting the Earth outside the atmosphere is subject neither to twinkling nor to light pollution from artificial light sources on the Earth.

Space-based astronomy is even more important for frequency ranges which are outside of the optical window and the radio window, the only two wavelength ranges of the electromagnetic spectrum that are not severely attenuated by the atmosphere. For example, X-ray astronomy is nearly impossible when done from the Earth, and has reached its current importance in astronomy only due to orbiting X-ray telescopes such as the Chandra observatory and the XMM-Newton observatory. Infrared and ultraviolet are also greatly blocked.

Space observatories can generally be divided into two classes: missions which map the entire sky (surveys), and observatories which make observations of chosen parts of the sky.

Many space observatories have already completed their missions, while others continue operating, and still others are planned for the future. Satellites have been launched and operated by NASA, ESA, Japanese Space Agency and the Soviet space program later succeeded by Roskosmos of Russia.

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