
Index 8. The Round Earth 8a. The Horizon 8b. Parallax 8c. Moon dist. (1) 8d. Moon dist. (2) 9a. Earth orbits Sun? 9c. Copernicus to Galileo 10. Kepler's Laws 10a. Scale of Solar Sys. 
Hipparchus, who used an eclipse of the Moon to deduce the precession of the equinoxes (here), used a total eclipse of the Sunprobably in 129 BCto estimate how far the Moon was. That distance had also been derived from a lunar eclipse by Aristachussee here. That eclipse was total at the Hellespontthe Dardanelles, part of the narrow strait that separates the European and Asian parts of Turkeybut only 4/5 of the Sun were covered in Alexandria of Egypt, further to the south. Hipparchus knew that when the Sun was eclipsed, it and the Moon occupied the same spot on the sphere of the heavens. The reason, he assumed, was that the Moon passed between us and the Sun. He believed that the Sun was much more distant than the Moon, as Aristarchus of Samos had concluded, about a century earlier, from observing the time when the Moon was exactly half full (see sections #8c and #9a).. He also assumed that the peak of the eclipse occured at the same time at both locations (not assured, but luckily not too far off), and he then carried out the following calculation. 
In a total eclipse of the Sun, the Moon just barely covers the Sun. The Sun itself is so distant that when viewed from anywhere on Earth, it covers practically the same patch of the sky, with a width of about 0.5°. Hipparchus concentrated on point E at the edge of the Moon (drawing), which during totality, when viewed from the Hellespont (point B) just overlapped point D on the edge of the Sun. Viewed from Alexandria (point A), at that same moment, the point E only overlapped point C on the Sun, about 1/5 solar diameter short of the edgewhich was why the eclipse there was not total. Onefifth of the Sun's diameter covers about 0.1° in the sky, so the small angle α (alpha, Greek A) between the two directions measured about 0.1 degrees. That angle is the parallax of the edge of the Moon, viewed from the above two locations. It is unlikely that Hipparchus knew the distance AB, but he probably knew the latitudes of the Hellespont and Alexandria. The local latitude can be shown to be equal to the elevation of the celestial pole above the horizon and today can be readily deduced by observing the height of Polaris, the pole star above the horizon. In the time of Hipparchus the pole of the heavens wasn't near Polaris (because of the precession of the equinoxes), but Hipparchus, who had mapped the positions of about 850 stars, must have known its position quite well. The latitude of the Hellespont (from a modern atlas) is about 40° 20' (40 degrees and 20 minutes, 60 minutes per degree), while that of Alexandria is about 31° 20', a difference of 9°. We will also assume Alexandria is exactly due south. If furthermore r is the radius of the Earth, then the circumference of the Earth 2πR, where π= 3.1415926... ("pi", Greek lowercase P) is the ratio between the circumference and diameter of any circle. Since the circumference also equals 360°, we get
where the dot marks multiplication (algebra's equivalent to the x symbol). The distance R to the MoonThe points AB are also located on another circle, centered on the Moon. The radius in that case is the distance R to the Moon, and because the arc AB covers 0.1°, we get
Multiplying both sides by 360 and dividing by 2π give
suggesting the Moon's distance is 90 Earth radii, an overestimate of about 50%. A more accurate calculationOne reason an excessive value was obtained is that the Moon was assumed to be overhead at A or B. Actually, it is likely to be at some significant angle to the overhead direction, the "zenith" (see drawing).Then the section cut by the angle α from the circle of radius R around E is not AB but AF (second drawing), which is smaller. Taking this into account reduces the distance. We don't know where the Sun was during the 129 BC eclipse, but it must have been on the ecliptic (the words are obviously related!), which places it within 23.5° of the celestial equator, on either side. Assuming it was on the equator (that is, it passed overhead on the Earth's equator) and south of the reported observations (i.e. the eclipse occured near noon) one can make a crude estimate of the correction, using simple trigonometry (see section M8). The Hellespont is around latitude of 40 degrees, and as the drawing shows, that is also the angle between the Moon's direction and the zenith. From the drawing (x marks multiplication)
Repeating the preceding calculation for AF
and in the end
NoteSome astronomers have questioned whether Hipparchus used the eclipse of 128 BCwhich occurred during his lifetimeor instead used records of an earlier one in 190 BC, which also passed not far from the Hellespont, along a very similar track. The paths of those eclipses and many others can be found in Fred Espenak's atlas of eclipses, accessible from the NASA eclipse page which he maintains, at
http://sunearth.gsfc.nasa.gov/eclipse/eclipse.html
Final commentsAccording to "A History of Astronomy" by A. Pannekoek, the result obtained by Hipparchus was between 62 and 73 Earth radii. Today we know the average distance is about 60 radii, varying by a few Earth radii either way because of the ellipticity of the Moon's orbit.In the absence of accurate timing, the method is almost guaranteed to produce an overestimate. The Earth rotates beneath the shadow spot cast by the Moon, which makes that spot sweep over a long strip, hitting many different locations at different times. The Hellespont was just one of many places where the eclipse was total. Similarly, Alexandria was just one of many locations where 4/5 of the Sun was covered. Randomly selecting point B from the first group and point A from the second may give a much longer baseline AB and a much larger (and incorrect) distance of the Moon. The fact Alexandria is almost exactly south of the Hellespont does not guarantee their peak eclipse times are the same, just that they are not too different.

Does history repeat itself?The total eclipse of the Sun on August 11, 1999 passed just a few hundred kilometers north of the one which Hipparchus used. Its path of totality extended from the ocean off New England, through England and central Europe, all the way across India. An eclipse map of the relevant area is shown on the rightthe double line outlines the region of totality, and the lines parallel to it give locations where 90%, 80% etc of the Sun were covered. As can be seen, the totality path crossed the Black Sea around 11:15 am Universal Time (1:15 pm local time) about 300 km. northeast of the Hellespont, and in Alexandria 71% of the Sun's diameter were covered (rather than 80% as in the Hipparchus eclipse) around 11:35 a.m.It will take a bit of work (a quicker way is sketched out at the bottom) but you can, if you wish, duplicate the calculation by Hipparchus for that eclipse (use a calculator, if possible) .

There also exists a quicker way. Note from the map that at the Hellespont 90% of the Sun was covered on 11 August 1999, which means that in one's field of view there, the front of the Moon's edge was 10% of the Sun's diameter from the edge of the Sun. In Alexandria the same argument shows the edge of the Moon 29% of the diameter from the edge. The lines of view from the two sites to the edge of the occulting Moon, at the height of the eclipse, therefore made an angle equal to 19% of the visual diameter of the Sunclose enough to the 20% which Hipparchus obtained! As the figure above shows, the path of totality on 11 August 1999 passed over Bucharest, the capital city of Romania. The Romanian government commemorated the event by drawing a map of the strip of totality over Romania (continuing the one drawn above) on its 2000Lei currency note. Click here to see a copy of that note (takes 132K of memory). Further details about this eclipse are available at http://sunearth.gsfc.nasa.gov/eclipse/TSE1999TSE1999.html. A comicstrip style site about the eclipse of 2.26.98, from "Sky and Telescope," gives many details applicable to solar eclipses in general. 
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Author and Curator: Dr. David P. Stern
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