Classifying the Source


 

Radiation whose direction can be identified is said to originate from a discrete source. A discrete source often can be associated with a visible (whether by the naked eye or by optical telescope) object. For example, a single star or small group of stars viewed from Earth is a discrete source. Our sun is a discrete source. A quasar is a discrete source. However, the definition of “discrete,” in addition to the other terms used to describe the extent of a source, often depends upon the beam size of the radio telescope antenna being used in the observation.

 

Discrete sources may be further classified as point sources, localized sources, and extended sources.

 

A point source is an idealization. It is defined as a source that subtends an infinitesimally small angle. All objects in reality subtend at least a very tiny angle, but often it is mathematically convenient for astronomers to regard sources of very small extent as point sources. Objects that appear smaller than the telescope’s beam size are often called “unresolved” objects and can effectively be treated as point sources. A localized source is a discrete source of very small extent. A single star may be considered a localized source.

 

Emitters of radiation that covers a relatively large part of the sky are called extended sources. An example of an extended source of radiation is our Milky Way galaxy, or its galactic center (called Sagittarius A) from which radiation emissions are most intense.

 

Classifying the Extent of the Source

 

source.jpg

 

An optical analogy to the extended source would be the view of a large city at night from an airplane at about 10 km altitude. All the city lights would tend to blend together into an appar-ently single, extended source of light. On the other hand, a single searchlight viewed from the same altitude would stand out as a single object, analogous to a localized or point source.

 

The terms localized and extended are relative and depend on the precision with which the telescope observing them can determine the source.

 

Background radiation is radio frequency radiation that originates from farther away than the object being studied, whereas foreground radiation originates from closer than the object being studied. If an astronomer is studying a specific nearby star, the radiation from the Milky Way may be considered not merely an extended source, but background radiation. Or, if it is a distant galaxy being observed, the Milky Way may be considered a pesky source of foreground radiation. Background and foreground radiation may consist of the combined emissions from many discrete sources or may be a more or less continuous distribution of radiation from our galaxy.

 

Cosmic background radiation, on the other hand, is predicted to remain as the dying glow from the big bang. It was first observed by Arno Penzias and Robert Wilson in 1965. (They won a Nobel Prize for this discovery in 1978). As discussed in Chapter 3, much of background and foreground radiation tends to be of non-thermal origin. The cosmic background radiation, however, is thermal.

 

In the group of pictures below (from Griffith Observatory and JPL), the entire sky is shown at (a) radio, (b) infrared, (c) visible, and (d) X-ray wavelengths. Each illustration shows the Milky Way stretching horizontally across the picture. It is clear that radio wavelengths give us a very different picture of our sky.

 

a.rc408_allsky.gif

 

b.iras_allsky.gif

 

c.opt2_allsky.gif

 

d.rosat_allsky.gif

 

 GBT Operations indexgenerate/gbt.gif

 



Basics of Radio Astronomy