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Astronomy Principles and Practice Fourth Edition.pdf

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so that we have<br />

But<br />

Hence,<br />

Similarly,<br />

ZC = ζ A + k tan ζ A ZD = ζ B + k tan ζ B .<br />

ZC = PC − PZ = 90 − δ − (90 − φ) = φ − δ.<br />

Atmospheric refraction 117<br />

φ − δ = ζ A + k tan ζ A . (10.9)<br />

ZD = ZP+ PD = 90 − φ + 90 − δ = 180 − φ − δ<br />

so that<br />

180 − φ − δ = ζ B + k tan ζ B . (10.10)<br />

If the observer’s latitude were accurately known, the two equations (10.9) <strong>and</strong> (10.10) in the two<br />

unknowns δ <strong>and</strong> k could be solved to yield values of δ <strong>and</strong> k. But because of small changes in the<br />

Earth’s crust, small variations take place in the latitude of the telescope used. In practice, therefore, at<br />

least two circumpolar stars are observed, within a short period of time, so that two more equations are<br />

obtained, namely<br />

φ − δ ′ = ζ A ′ + k tan ζ A ′ . (10.11)<br />

180 − φ − δ ′ = ζ B ′ + k tan ζ B ′ . (10.12)<br />

The four equations (10.9)–(10.12) are now solved to give values of δ, δ ′ , φ <strong>and</strong> k.<br />

10.2.4 Horizontal refraction<br />

When the Sun or Moon is observed rising or setting, the observed zenith distance of its centre is 90 ◦ .<br />

For such a zenith distance, the refraction amounts to 35 ′ <strong>and</strong> is called the horizontal refraction. Since<br />

the angular diameter of these bodies is about 30 ′ , they are, in fact, below the horizon when their centres<br />

are seen to be on the horizon. In the case of the Sun, therefore, horizontal refraction lengthens the time<br />

interval during which it is daylight, sunrise <strong>and</strong> sunset taking place earlier <strong>and</strong> later respectively than<br />

they would occur if refraction were absent. Tables which provide accurate sunrise <strong>and</strong> sunset times for<br />

any location take account of horizontal refraction—a point not mentioned in section 8.11.<br />

Table 10.1 shows how quickly refraction diminishes with altitude. Because of this, an extended<br />

body like the Sun is decidedly oval in shape near rising <strong>and</strong> setting, the refraction of the upper <strong>and</strong><br />

lower limbs being different.<br />

Table 10.1. Variation of apparent altitude with angle of refraction.<br />

Apparent altitude<br />

Angle of refraction<br />

0 ◦ 35 ′ 21 ′′<br />

1 ◦ 24 ′ 45 ′′<br />

2 ◦ 18 ′ 24 ′′<br />

3 ◦ 14 ′ 24 ′′<br />

4 ◦ 11 ′ 43 ′′<br />

10 ◦ 5 ′ 18 ′′<br />

30 ◦ 1 ′ 41 ′′<br />

60 ◦ 0 ′ 34 ′′<br />

90 ◦ 0 ′ 0 ′′

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