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OF THE ROGER N. CLARK

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VISUAL ASTRONOMY <strong>OF</strong> <strong>THE</strong> DEEP SKY<br />

<strong>THE</strong> HUMAN EYE<br />

Since astronomical objects cover an area of<br />

sky, their surface brightnesses are described<br />

in magnitudes per square arc-second. The<br />

full Moon, fo r example, is a half degree (1800<br />

arc-seconds) in diameter, so it covers 2.5 million<br />

square arc-seconds of sky. Dividing its<br />

brightness by its area gives it a surface<br />

brightness of 3.6 magnitudes per square arcsecond.<br />

Astronomical objects differ vastly in both<br />

total brightness and surface brightness. The<br />

full Moon and the planet Mars have nearly<br />

the same surface brightness; their total<br />

amounts of light are so different only because<br />

the Moon covers a much larger area of sky.<br />

The Moon and the Sun, on the other hand,<br />

have nearly the same apparent size. Here it's<br />

a difference in surface brightness that causes<br />

such dissimilar amounts of light.<br />

An object of a certain total brightness<br />

(such as the Moon) also illuminates the surface<br />

of the Earth with a certain number of<br />

lumens per square meter. Any astronomical<br />

object illuminates the Earth's surface in such<br />

a manner. Examples are in Table 2.1.<br />

The illumination an object causes on the<br />

Earth's surface is directly relevant to astronomy.<br />

A telescope objective has a given area<br />

on which light from the object falls. The illumination<br />

per unit area times the area of the<br />

;:--<br />

E 160<br />

E<br />

140<br />

..<br />

Cl)<br />

Q.. 120<br />

(I)<br />

"0<br />

c::<br />

ctI<br />

(I)<br />

::3<br />

0<br />

..c:::<br />

-<br />

100<br />

80<br />

60<br />

0:<br />

40<br />

LU<br />

CO 20<br />

<br />

0<br />

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