| Theory of the Moon – First inequality | |
| Book IV of the "Almagest"
is dedicated to an "elementary" theory of the Moon, namely, to a
simple kinetic model that assumes the Moon moving (with a retrograde motion)
on an epicycle moving (with a direct motion) on a deferent, on which the
observer is centrally positioned.
This model should be the exact kinetic equivalent of the Sun’s motion model, except for two characteristics which are peculiar to the Lunar theory: |
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| a) | the apsidal line of the orbit of the Moon rotates (with a direct motion) |
| b) | the orbit of the Moon, i.e. the common plane of the deferent and of the epicycle, is inclined to the ecliptic. Anyway, as the value of the angle of this inclination is small (5°), it will not be considered for the computation of longitude. The latitudes can be computed independently, using the same method used for the solar declination. |
| The "elementary"
theory of the Moon’s motion is, for sure, the greatest contribution of
theoretical astronomy that Ptolemy inherited from his predecessors. Anyway,
a careful analysis of the grounds on which classical theory was developed,
drove him to significant numerical and methodological improvements.
The theory developed up to this moment is based on data achieved from the eclipses of the Moon. Book V of the Almagest shows that the longitudes of the Moon, different than those of the syzygies, are not represented with sufficient accuracy. It also puts into evidence a "second anomaly" of the Moon’s motion, which depends from the elongation of the Moon with respect to the Sun. This anomaly is zero at syzygies, therefore, the elementary theory of Book IV is valid for the theory of the eclipses. The second anomaly, known today as "evection", had a vast influence on the techniques of the ancient and medieval astronomers through the invention of Ptolemy of mobile eccenters by which he succeeded to correctly describe the deviations observed with respect to the elementary theory. In accordance with these improvements in the theory of the motion of the Moon’s positions, the most accurate known data for the determination of the nearby positions of planets and fixed stars were provided. Effectively, the parameters of the theory of the Moon originate from the eclipses, because only with the use of the solar theory the ecliptic coordinates are known with enough accuracy. The above underlines the crucial importance of theoretical models and of their correlation (in the order) with the Sun, the Moon, the Planets and the Fixed Stars (which, in turn, influence the determination of the sidereal and tropical coordinates), showing its major importance with respect to individual observations. This unbalance between theoretical structures and direct observations increased more and more post Ptolemy’s times and is a peculiarity of all the pre-telescopic astronomy. In Chap. 1 of Book IV Ptolemy explains that only the eclipses of the Moon are useful for the determination of the longitudes of the Moon as they are independent from the parallax. Chap. 2 gives a brief historical summary concerning the determination of the fundamental relations between the periods of the motions of the Moon, followed by a critical discussion of the method to determine the length of the anomalistic period. Chap. 3 derives the numerical values of the different mean motions, afterwards tabulated in Chap. 4. Ptolemy inherits from Hipparchus the following parameters: |
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| a) | Mean Synodic Month: 29;31,50,8,20 days |
| b) | 251 Synodic Months = 269 Anomalistic Months |
| d) | 5458 Synodic Months = 5923 Periods of Latitude |
| d) | sexagesimally: 4,11 Synodic Months = 4,29 Anomalistic Months |
| e) | sexagesimally: 1,30,58 Synodic Months = 1,38,43 Periods of Latitude |
| We saw that the anomaly
of the Sun was determined in Greek astronomy by the disparity of the seasons.
Such a simple method does not exist for the Moon because of its short anomalistic
period of about 27,5 days. It is difficult to imagine an alternative other
than that of discovering the variability of the velocity of the Moon by
observing, day after day, the motion of the Moon with respect to the fixed
stars. The existence of such observation is greatly certified in the "Babylonian
Diaries" of the Persian and of the Seleucid period; it is therefore
not surprising that very accurate values of the length of the anomalistic
month, integrated in the computation of the Babylonian ephemerides can
be found.
The historical introduction of Ptolemy to Book
IV of the Almagest shows, in an evident way, that Babylonian parameters
were known to Hipparchus. For him, the problem consisted in testing these
Babylonian parameters and in obtaining values the most accurate possible,
for the mean anomalistic motion. Ptolemy assumes that only the eclipses
of the Moon are sufficiently accurate for the determination of the longitudes
of the Moon.
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| Theory of the Moon – Second inequality | |
| As seen in the previous section,
the determination of the characteristic features of the theory of the Moon
are derived from the observation of the eclipses. Particularly, the Babylonian
values and those of Hipparchus, relevant to the mean motions in longitude,
anomaly and latitude had at their back nearly six centuries of records
of eclipses. It is therefore not surprising that, both Hipparchus and Ptolemy,
found a good correspondence between data predicted and data observed, both
relevant to the eclipses of the Moon.
Therefore, the "elementary" epicycle model that produces the first inequality shows satisfactory for the prediction of the eclipses. But as known from the introduction to Chap. 2 of Book V of the Almagest, Hipparchus found significant deviations from the predicted longitudes for the Moon positions not associated with the syzygies, particularly near to the quadratures. To all appearances, however, these discrepancies were too irregular, both in value and in position, and enough not to allow Hipparchus to build up a self-consistent theoretical picture of the motion of the Moon. Ptolemy, aware of these deviations, undertook a systematic study of the observational evidence, succeeding in the task of discovering the structure of these perturbations. Such study involved a great work of calculation, since he would have not been able to reach his conclusions without computing in each single case, the mean longitudes of the Sun and of the Moon, the anomaly of the Moon and the effects of the longitudinal components on the parallax of the Moon. The structure that Ptolemy draws from the numerical
data is summarized in the following statements:
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| 1) | absence of deviations (or, at the limit, deviations within values justifiable by the parallax) in the syzygies |
| 2a) | absence, or only small deviations in the quadratures, under the condition that the Moon is simultaneously near to the apogee or to the perigee of the epicycle |
| 2b) | maximum deviation in the quadratures when, the Moon is at the same time, near to the maximum equation caused by the epicycle anomaly |
| Ptolemy realized that exactly this
type of discrepancies from the elementary theory would have been explained
by an increase of the radius of the epicycle in the quadratures, with respect
to the syzygies, as previously confirmed by the eclipses.
A dynamic variation in the measure of the epicycle would contradict the spirit of the kinetic models of the Greek astronomy. Anyway the same effect could be obtained moving the epicycle near to the observer when in quadrature, apparently increasing its size. Consequently, Ptolemy imposed an eccentric independent motion to the deferent of the orbit of the Moon, connected with the elongation with regard to the Sun. At conjunctions and oppositions the centre C of the epicycle remains at its original distance = 60 from the observer O, while at elongations 90° and 270° the distance OC must be reduced to the value required by the observed maximum increment of the epicycle equation. The kinetic device created by Ptolemy, to obtain such a periodic variation of the distance, consists in a mechanism of the type: crank -connecting rod. The effect produced by this innovative model on the longitude of the Moon, not regulated by the "elementary" model, is known as the "second inequality". It generally identifies the periodic inequality that in modern celestial dynamic is known as "evection", to which Tycho Brahe added another term, the "variation", that reaches its maximum between the syzygies and the quadratures, being zero at both these points. A similar term occurs also in Ptolemy’s model of the Lunar motion. Bibliography: O. Neugebauer - "A History of Ancient Mathematical Astronomy" - Springer |
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