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Astronomy Principles and Practice Fourth Edition.pdf

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126 The reduction of positional observations: I<br />

near the observer’s meridian at midnight. Observations are made a few hours before midnight <strong>and</strong><br />

a few hours after midnight. Before the development of radar, many observatories carried out such<br />

observing programmes, notably between 1900 <strong>and</strong> 1901 <strong>and</strong> between 1930 <strong>and</strong> 1931, when Eros was<br />

in opposition. The value of the solar parallax (see section 10.4) derived from these programmes was<br />

probably not any more accurate than one part in a thous<strong>and</strong>.<br />

Nowadays, the use of powerful radio telescopes as radar telescopes has enabled the accuracy to<br />

be increased by a factor of at least one hundred. The geocentric distance of the planet Venus has been<br />

measured repeatedly by this method. It consists essentially of timing the interval between transmission<br />

of a radar pulse <strong>and</strong> the reception of its echo from Venus. This interval, with a knowledge of the velocity<br />

of electromagnetic radiation (the speed of light) enables the Earth–Venus distance to be found. Thus,<br />

if EV, c <strong>and</strong> t are the Earth–Venus distance, velocity of radio waves <strong>and</strong> time interval respectively,<br />

EV = 1 2 ct.<br />

Various corrections have to be made to derive the distance Venus-centre to Earth-centre. For<br />

example, the distance actually measured is the distance from the telescope to the surface of Venus. The<br />

effect of the change of speed of the radar pulse when passing through the ionosphere also has to be<br />

taken into account.<br />

An even more accurate value of the solar parallax has been obtained by tracking Martian artificial<br />

satellites such as Mariner 9 over extended periods of time. Range <strong>and</strong> range rate measurements (i.e.<br />

line of sight distance <strong>and</strong> speed by radio tracking) allow the distance Earth-centre to Mars-centre to be<br />

found.<br />

10.7 Stellar parallax<br />

10.7.1 Stellar parallactic movements<br />

The direction of a star as seen from the Earth is not the same as the direction when viewed by a<br />

hypothetical observer at the Sun’s centre. As the Earth moves in its yearly orbit round the Sun, the<br />

geocentric direction (the star’s position on a geocentric celestial sphere) changes <strong>and</strong> traces out what is<br />

termed the parallactic ellipse. Thus, in figure 10.10, the star X at a distance d kilometres is seen from<br />

the Earth at E 1 to lie in the direction E 1 X 1 relative to the heliocentric direction SX ′ . Six months later,<br />

the Earth is now at the point E 2 in its orbit <strong>and</strong> the geocentric direction of the star is E 2 X 2 .<br />

The concepts used in stellar parallax are analogous to those used in geocentric parallax. Thus, if<br />

we looked upon the Earth’s orbital radius a as the base-line, we can define the star’s parallax as P,<br />

given by<br />

sin P = a d . (10.30)<br />

Because stellar distances are so great compared with the Earth’s orbital radius, we can assume<br />

that the Earth’s orbit to be circular. Angle P is small so that we can write equation (10.30) as<br />

P = 206 265 a d<br />

where P is in seconds of arc.<br />

Again, if we draw E 1 Y parallel to SX in figure 10.10 <strong>and</strong> let YE 1 X = E 1 XS = p, wehave,<br />

from △E 1 XS,<br />

sin p<br />

= sin XE 1S<br />

a d<br />

or<br />

sin p = a d sin XE 1S.

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