Great Astronomers eBook

This eBook from the Gutenberg Project consists of approximately 318 pages of information about Great Astronomers.

Great Astronomers eBook

This eBook from the Gutenberg Project consists of approximately 318 pages of information about Great Astronomers.
years.  The actual effect which is produced by the lunar acceleration, for so this phenomenon is called, may be thus estimated.  If we suppose that the moon had, throughout the ages, revolved around the earth in precisely the same periodic time which it has at present, and if from this assumption we calculate back to find where the moon must have been about two thousand years ago, we obtain a position which the ancient eclipses show to be different from that in which the moon was actually situated.  The interval between the position in which the moon would have been found two thousand years ago if there had been no acceleration, and the position in which the moon was actually placed, amounts to about a degree, that is to say, to an arc on the heavens which is twice the moon’s apparent diameter.

If no other bodies save the earth and the moon were present in the universe, it seems certain that the motion of the moon would never have exhibited this acceleration.  In such a simple case as that which I have supposed the orbit of the moon would have remained for ever absolutely unchanged.  It is, however, well known that the presence of the sun exerts a disturbing influence upon the movements of the moon.  In each revolution our satellite is continually drawn aside by the action of the sun from the place which it would otherwise have occupied.  These irregularities are known as the perturbations of the lunar orbit, they have long been studied, and the majority of them have been satisfactorily accounted for.  It seems, however, to those who first investigated the question that the phenomenon of the lunar acceleration could not be explained as a consequence of solar perturbation, and, as no other agent competent to produce such effects was recognised by astronomers, the lunar acceleration presented an unsolved enigma.

At the end of the last century the illustrious French mathematician Laplace undertook a new investigation of the famous problem, and was rewarded with a success which for a long time appeared to be quite complete.  Let us suppose that the moon lies directly between the earth and the sun, then both earth and moon are pulled towards the sun by the solar attraction; as, however, the moon is the nearer of the two bodies to the attracting centre it is pulled the more energetically, and consequently there is an increase in the distance between the earth and the moon.  Similarly when the moon happens to lie on the other side of the earth, so that the earth is interposed directly between the moon and the sun, the solar attraction exerted upon the earth is more powerful than the same influence upon the moon.  Consequently in this case, also, the distance of the moon from the earth is increased by the solar disturbance.  These instances will illustrate the general truth, that, as one of the consequences of the disturbing influence exerted by the sun upon the earth-moon system, there is an increase in the dimensions of the average orbit which the moon describes around the earth.  As the time required by the moon to accomplish a journey round the earth depends upon its distance from the earth, it follows that among the influences of the sun upon the moon there must be an enlargement of the periodic time, from what it would have been had there been no solar disturbing action.

Copyrights
Project Gutenberg
Great Astronomers from Project Gutenberg. Public domain.