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Astronomy Principles and Practice Fourth Edition.pdf

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The role of the observer 17<br />

Earth <strong>and</strong> on micrometeoritic material which is scooped up by rocket probes in the upper atmosphere.<br />

Some thirty years ago the Apollo <strong>and</strong> Lunakhod missions brought back our first samples of lunar<br />

material for laboratory study. Interplanetary space probes have sent <strong>and</strong> still are sending back new data<br />

from the experiments which they carry. They are able to transmit information about the planets that<br />

could not have been gained in any other way. Astronomers have also gleaned information about the<br />

planets by using radar beams. However, all these active experiments <strong>and</strong> observations are limited to<br />

the inner parts of the Solar System, to distances from the Earth which are extremely small in relation<br />

to distances between the stars.<br />

When it comes to stellar work, the experiments, whether on board space vehicles or Earth<br />

satellites, or at the bottom of the Earth’s atmosphere, are more passive. They involve the measurement<br />

<strong>and</strong> analysis of radiation which happens to come from a particular direction at a particular time. It is<br />

very true to say that practically the whole of the information <strong>and</strong> knowledge which has been built up of<br />

the outside Universe has been obtained in this way, by the patient analysis of the energy which arrives<br />

constantly from space.<br />

As yet, the greater part of this knowledge has been built up by the observer using ground-based<br />

telescopes though in recent years a wide variety of artificial satellite-based telescopes such as the<br />

Hubble Space Telescope <strong>and</strong> Hipparcos have added greatly to our knowledge. The incoming radiation<br />

is measured in terms of its direction of arrival, its intensity, its polarization <strong>and</strong> their changes with time<br />

by appending analysing equipment to the radiation collector <strong>and</strong> recording the information by using<br />

suitable devices. The eye no longer plays a primary role here. If the radiation has passed through the<br />

Earth’s atmosphere, the measurements are likely to have reduced quality, in that they are subject to<br />

distortions <strong>and</strong> may be more uncertain or exhibit an increase of noise. In most cases, however, these<br />

effects can be allowed for, or compensated for, at least to some degree.<br />

The task of the observer might be summarized as being one where the aim is to collect data<br />

with maximum efficiency, over the widest spectral range, so that the greatest amount of information<br />

is collected accurately in the shortest possible time, all performed with the highest possible signal-tonoise<br />

ratio. Before the data can be assessed, allowances must be made for the effects of the radiation’s<br />

passage through the Earth’s atmosphere <strong>and</strong> corrections must be applied because of the particular<br />

position of the observer’s site <strong>and</strong> the individual properties of the observing equipment.<br />

It may be noted here also that with the advent of computers, more <strong>and</strong> more observational work is<br />

automated, taking the astronomer away from the ‘h<strong>and</strong>s-on’ control of the telescope <strong>and</strong> the interface<br />

of the data collection. This certainly takes away some of the physical dem<strong>and</strong>s made of the observer<br />

who formally operated in the open air environment of the telescope dome sometimes in sub-zero<br />

temperatures. Accruing data can also be assessed in real time so providing instant estimates as to<br />

its quality <strong>and</strong> allowing informed decisions to be made as to how the measurements should proceed.<br />

In several regards, the application of computers to the overall observational schemes have made the<br />

data more objective—but some subtleties associated with operational subjectivity do remain, as every<br />

computer technologist knows.<br />

We cannot end this chapter without mentioning the role of the theoretical astronomers. Part of<br />

their tasks is to take the data gathered by the observers <strong>and</strong> use them to enlarge <strong>and</strong> clarify our picture<br />

of the Universe. Their deductions may lead to new observational programmes which will then support<br />

their theories or cast doubt upon their validity.<br />

Several comments may be made here.<br />

It goes without saying that an astronomer may be both theoretician <strong>and</strong> observer, though many<br />

workers tend to specialize in one field or the other. Again, it has been estimated that for each hour of<br />

data collecting, many hours are spent reducing the observations, gleaning the last iota of information<br />

from them <strong>and</strong> pondering their relevance in our efforts to underst<strong>and</strong> the Universe. The development of<br />

astronomical theories often involves long <strong>and</strong> complicated mathematics, in areas such as celestial mechanics<br />

(the theory of orbits), stellar atmospheres <strong>and</strong> interiors <strong>and</strong> cosmology. Happily in recent years,<br />

the use of the ubiquitous computer has aided tremendously the theoretician working in these fields.

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