Radio and radar astronomyradar astronomy
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What is radio astronomy?
Radio astronomy uses radio receivers and antenna systems, known as radio telescopes, to detect radio-frequency radiation from extraterrestrial sources like stars, galaxies, and quasars. These telescopes help astronomers study various objects by measuring temperatures of planets and moons, mapping the surface of Venus, and testing Einstein's theory of general relativity.
Radio telescopes consist of a large radio antenna and a sensitive radio receiver. They can measure weak sources of radio emission, and are protected from man-made emissions. Radio astronomers have discovered about 150 molecules, and can also measure the change in the wavelength of observed lines arising from the Doppler effect.
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How is radar astronomy different from radio astronomy?
Both radio astronomy and radar astronomy study celestial bodies using radio frequencies, but they do so in different ways. Radio astronomy involves the examination of the radio-frequency energy that objects emit naturally. In contrast, radar astronomy studies solar system objects by analyzing radio waves that are directed at them and then reflected back.
Radio telescopes can measure surface temperatures of planets and detect molecules in space. Radar systems can measure the distance to objects in the solar system and image their surfaces.
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What kinds of objects in space can radio astronomers study?
Radio telescopes enable astronomers to investigate various extraterrestrial radio sources that emit radio waves through multiple processes. These objects include planets, moons, stars, and galaxies.
Radio astronomers can study thermal radiation from solid bodies, such as planets, and thermal radiation from hot gas in the interstellar medium. They also study synchrotron emission from electrons moving near light speed in weak magnetic fields and spectral line radiation from atomic or molecular transitions in the interstellar medium or gaseous envelopes around stars. Pulsed radiation from rapidly rotating neutron stars with intense magnetic fields and energetic electrons can also be studied.
Radio telescopes can detect neutral hydrogen, revealing the structure and motion of the Milky Way. They have also facilitated the discovery of about 150 molecules, such as water and alcohol. Additionally, they allow the study of powerful radio galaxies and quasars far beyond the Milky Way.
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What equipment do scientists use in radio and radar astronomy?
Radio and radar astronomy relies on specialized equipment to study celestial bodies by examining the radio-frequency energy they emit or reflect. The key instruments include:
- Radio Telescopes: These consist of a large radio antenna and a sensitive radiometer, or radio receiver. The most familiar type is the radio reflector, which has a parabolic antenna that focuses incoming radiation onto a feed. To achieve the best possible sensitivity, solid-state amplifiers are used and cooled to very low temperatures to reduce internal noise.
- Radio Interferometers: These are made up of two or more separate antennas that receive radio waves from the same astronomical object and are connected to the same receiver. A variable-delay mechanism compensates for the time difference in the arrival of radio waves at the spaced antennas, allowing the waves to interfere.
- Radar Systems: Powerful radar systems are used to detect radio signals reflected from nearby astronomical bodies. Measurements of the time delay and spectrum of the returned signal enable precise determination of distances and imaging of surface features.
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How does radar help scientists learn about planets or asteroids?
Radar helps scientists study planets and asteroids by using radio telescopes to examine the radio-frequency energy that celestial bodies emit or reflect. Radar techniques measure the spectrum and flight time of signals reflected from planetary surfaces, which allows scientists to examine topographical features with a linear resolution as good as 1 km, deduce rates of rotation, and determine the distance to planets with great accuracy. Because radio wavelengths can penetrate planetary atmospheres, radar is an effective means of probing a planet’s surface.
Radar has been used to study the Moon, Venus, and near-Earth asteroids. For example, radar echoes from Venus have penetrated its dense cloud cover and uncovered valleys and enormous mountains on the planet's surface.
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What important discoveries have been made using radio or radar astronomy?
Radio and radar astronomy have led to many important discoveries. Karl Jansky detected cosmic radio noise from the Milky Way in 1932. Later, Grote Reber built the first radio telescope and found radio radiation from the Milky Way and the Sun.
Radio telescopes have been used to measure the surface temperatures of planets and moons. Radar measurements determined Mercury's rotation. Radio waves have also revealed features on Venus's surface, which is obscured by clouds.
In 1967, the discovery of pulsars (rapidly rotating neutron stars) revealed the existence of these stars throughout the Milky Way Galaxy. Arno Penzias and Robert Wilson detected cosmic microwave background radiation, the remaining radiation from the big bang.
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Radio and radar astronomyradar astronomy, study of celestial bodies by examination of the radio-frequency energy they emit or reflect. Radio waves penetrate much of the gas and dust in space, as well as the clouds of planetary atmospheres, and pass through Earth’s atmosphere with little distortion. Radio astronomers can therefore obtain a much clearer picture of stars and galaxies than is possible by means of optical observation. The construction of ever larger antenna systems and radio interferometers (see telescope: Radio telescopes) and improved radio receivers and data-processing methods have allowed radio astronomers to study fainter radio sources with increased resolution and image quality.
In 1932 the American physicist Karl Jansky first detected cosmic radio noise from the centre of the Milky Way Galaxy while investigating radio disturbances that interfered with transoceanic telephone service. (The radio source at the centre of the Galaxy is now known as Sagittarius A.) The American amateur radio operator Grote Reber later built the first radio telescope at his home in Wheaton, Ill., and found that the radio radiation came from all along the plane of the Milky Way and from the Sun. For the first time, astronomers could observe objects in a new region of the electromagnetic spectrum outside that of visible light.
During the 1940s and ’50s, Australian and British radio scientists were able to locate a number of discrete sources of celestial radio emission that they associated with old supernovae (Taurus A, identified with the Crab Nebula) and active galaxies (Virgo A and Centaurus A) that later became to be known as radio galaxies.
In 1951, American physicists Harold Ewen and E.M. Purcell detected 21-cm radiation emitted by cold clouds of interstellar hydrogen atoms. This emission was later used to define the spiral arms of the Milky Way Galaxy and to determine the rotation of the Galaxy.
In the 1950s, astronomers at Cambridge University published three catalogs of astronomical radio sources. The last of these, the Third Cambridge Catalogue (or 3C), published in 1959, contained some sources, most notably 3C 273, that were identified with faint stars. In 1963 American astronomer Maarten Schmidt observed 3C 273 with an optical telescope and found that it was not a star in the Milky Way Galaxy but a very distant object nearly two billion light-years from Earth. Objects like 3C 273 were called quasi-stellar radio sources, or quasars.
Beginning in the late 1950s, radio studies of the planets revealed the existence of a greenhouse effect on Venus, intense Van Allen radiation belts surrounding Jupiter, powerful radio storms in Jupiter’s atmosphere, and an internal heating source deep within the interiors of Jupiter and Saturn.
Radio telescopes are also used to study interstellar molecular gas clouds. The first molecule detected by radio telescopes was hydroxyl (OH) in 1963. Since then about 150 molecular species have been detected, only a few of which can be observed at optical wavelengths. These include carbon monoxide, ammonia, water, methyl and ethyl alcohol, formaldehyde, and hydrogen cyanide, as well as some heavy organic molecules such as the amino acid glycine.
In 1964, Bell Laboratories scientists Robert Wilson and Arno Penzias detected the faint cosmic microwave background (CMB) signal left over from the original big bang, thought to have occurred 13.8 billion years ago. Subsequent observations of this CMB in the 1990s and 2000s with the Cosmic Background Explorer and the Wilkinson Microwave Anisotropy Probe satellites have detected fine-scale deviations from the smooth background that correspond to the initial formation of structure in the early universe.
Radio observations of quasars led to the discovery of pulsars (or pulsating radio stars) by British astronomers Jocelyn Bell and Antony Hewish in Cambridge, Eng., in 1967. Pulsars are neutron stars that spin very rapidly, up to nearly 1,000 times per second. Their radio emission is concentrated along a narrow cone, producing a series of pulses corresponding to the rotation of the neutron star, much like the beacon from a rotating lighthouse lamp. In 1974, using the Arecibo Observatory, American astronomers Joseph Taylor and Russell Hulse observed a binary pulsar (two pulsars in orbit around each other) and found that their orbital period was decreasing because of gravitational radiation at exactly the rate predicted by Albert Einstein’s theory of general relativity.
Using powerful radar systems, it is possible to detect radio signals reflected from nearby astronomical bodies such as the Moon, the nearby planets, some asteroids and comets, and the larger moons of Jupiter. Precise measurements of the time delay between the transmitted and reflected signal and the spectrum of the returned signal are used to precisely measure the distance to solar system objects and to image their surface features with a resolution of a few metres. The first successful detection of radar signals from the Moon occurred in 1946. This was quickly followed by experiments in the United States and the Soviet Union using powerful radar systems built for military and commercial applications. Both radio and radar studies of the Moon revealed the sandlike nature of its surface even before the Apollo landings were made. Radar echoes from Venus have penetrated its dense cloud cover surrounding the surface and have uncovered valleys and enormous mountains on the planet’s surface. The first evidence for the correct rotation periods of Venus and of Mercury also came from radar studies.


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