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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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color excess<br />

color excess A measure of the reddening<br />

of starlight due to small intervening interstellar<br />

dust grains. It has been found for most interstellar<br />

dust clouds that the extinction of light is<br />

proportional to the amount of reddening that a<br />

given interstellar cloud causes.<br />

AV<br />

E<br />

= 3.2 .<br />

AV is the visual extinction (obscuration) of light<br />

in magnitudes, <strong>and</strong> E is the color excess of B <strong>and</strong><br />

V magnitudes, given by the intrinsic color index<br />

subtracted from the measured color index<br />

E=(B −V)−(B −V)o<br />

where (B−V) <strong>and</strong> (B−V)o are the measured <strong>and</strong><br />

expected color indices, respectively, of a star of<br />

a known temperature (see color index). Since<br />

the ratio of extinction to reddening is known,<br />

then the luminosity of the star can be derived<br />

<strong>and</strong> hence the distance to the star.<br />

color index The difference between a star’s<br />

apparentmagnitudeatsomegivenwavelengthto<br />

that at another (longer) wavelength. A typical<br />

color index used is B–V, where B <strong>and</strong> V are the<br />

apparent blue <strong>and</strong> visible magnitudes measured<br />

with st<strong>and</strong>ard filters at 4200 <strong>and</strong> 5400, respectively.<br />

The color index is independent of distance<br />

<strong>and</strong> gives a measure of a star’s color temperature,<br />

that temperature which approximates<br />

the radiation distribution of the star as a black<br />

body(seecolortemperature). Foranygivenstellar<br />

type, there is an expected color index, calculated<br />

by assuming a black body temperature for<br />

the star. Any difference between the observed<br />

color index <strong>and</strong> the measured color index of a<br />

star is due to interstellar reddening. See color<br />

excess.<br />

color-magnitude diagram See HR (Hertzsprung–Russell)<br />

diagram.<br />

color temperature The temperature that describes<br />

a black body radiation distribution based<br />

on the intensity ratios at two or more wavelength<br />

intervals (or “colors”). One reason that the radiation<br />

distribution from stars deviates from that<br />

of a black body is that atoms <strong>and</strong> molecules in<br />

the stellar atmosphere deplete radiation from the<br />

© 2001 by CRC Press LLC<br />

continuum for spectral line formation. Then a<br />

least squares fit of a Planck curve to the stellar<br />

spectrum will underestimate the radiation temperature<br />

of the star. However, since the shape<br />

of a black body curve for any temperature is the<br />

same, the ratio of the intensity at two wavelength<br />

intervals judiciously chosen to avoid strong absorption<br />

features will give a temperature that<br />

more closely describes the radiation distribution<br />

that the star is actually putting out.<br />

coma In a comet, the region of heated gas<br />

<strong>and</strong> dust surrounding the nucleus of the comet,<br />

distinct from the tails which are generated by<br />

nuclear <strong>and</strong> coma material driven off by solar<br />

wind <strong>and</strong> solar radiation pressure. The gas in<br />

the coma may be ionized, <strong>and</strong> its composition<br />

can vary with distance from the comet as the<br />

different molecules undergo photo-dissociation<br />

with time. The coma can reach many millions of<br />

kilometers in radius. In optics, an image defect<br />

in which the image of a point consists of an offcenter<br />

bright spot in a larger, fainter “coma”.<br />

comet A small solar system object composed<br />

substantially of volatile material, which is distinctive<br />

because of its rapid motion across the<br />

sky <strong>and</strong> its long tail(s) of gas <strong>and</strong> dust emitted<br />

from the body. An accurate description of<br />

a comet is a “dirty snowball”, “dirty iceberg”<br />

since comets contain some rocky material but<br />

are primarily composed of ice. The rocky-icy<br />

center of a comet is called the nucleus. Comets<br />

usually orbit the sun in highly elliptical orbits.<br />

As the comet nears the sun, the increased temperature<br />

causes the ice in the nucleus to sublimate<br />

<strong>and</strong> form a gaseous halo around the nucleus,<br />

called the coma. Comets often possess<br />

two tails: a dust tail that lies in the orbit behind<br />

the comet generated by surface activity,<br />

<strong>and</strong> a brighter, ionized gas tail, that points away<br />

from the sun, driven by solar wind. Long period<br />

comets (periods greater than 200 years) are<br />

thought to originate in the Oort cloud, a spherical<br />

shell surrounding the Earth at distances exceeding<br />

50,000 AU. They are perturbed by the planets<br />

(especially Jupiter) to fall in toward the sun.<br />

Their orbits typically have r<strong>and</strong>om inclinations<br />

<strong>and</strong> very large eccentricities; some hyperbolic<br />

orbits have been observed. Short period comets<br />

apparently arise in the Kuiper Belt, in the zone

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