mysteries of egyptian zodiacs - HiddenMysteries Information Central
mysteries of egyptian zodiacs - HiddenMysteries Information Central
mysteries of egyptian zodiacs - HiddenMysteries Information Central
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136 6 Method <strong>of</strong> Astronomical Determination <strong>of</strong> the Dates Encoded in Egyptian Zodiacs<br />
with the year 4713 B.C,, J. Scaliger decided to number all<br />
the days. For example the Julian day <strong>of</strong> April 1, 1400 A.D.,<br />
corresponds to the number 2232407 4 .<br />
Figure 6.2: The celestial sphere with the indicated ecliptic,<br />
equator, and the equinox and solstice points. The spring and<br />
autumn equinox points are the intersection points <strong>of</strong> the ecliptic<br />
with the equator.<br />
On Figure 6.2, besides the ecliptic there is another large<br />
circle marked on the celestial sphere, which is the equator.<br />
This equator is exactly the intersection circle <strong>of</strong> the plane<br />
containing the Earth’s equator with the celestial sphere. It<br />
is a well-known fact, that the equator circle is relatively fast<br />
changing its position in time. It constantly revolves around<br />
the celestial sphere.<br />
The ecliptic and equator intersect on the celestial sphere<br />
at the angle <strong>of</strong> 23 o 27 ′ approximately. The points <strong>of</strong> their intersection<br />
are denoted on Figure 6.2 by the letters Q and R.<br />
In the course <strong>of</strong> a year, the Sun in its apparent movement<br />
along the ecliptic crosses twice the equator at these points.<br />
The point Q, through which the Sun enters into the northern<br />
hemisphere, is called the spring equinox point. At that<br />
time the day and night are <strong>of</strong> equal length. The opposite to<br />
Q point on the celestial sphere is the autumn equinox point.<br />
On Figure 6.2, this point is denoted by the letter R. Through<br />
the point R the Sun enters the southern hemisphere. At that<br />
time the day and night are again <strong>of</strong> equal length.<br />
4 See [27], p. 316.<br />
The winter and summer solstice points are also located on<br />
the ecliptic. The four equinox and solstice points divide the<br />
ecliptic into four equal parts (see Figure 6.2).<br />
As time goes by, the four equinox and solstice points continually<br />
move along the ecliptic in the direction <strong>of</strong> decreasing<br />
ecliptic longitude. This motion is called in astronomy the<br />
precession <strong>of</strong> the equinoxes or simply the precession 5 . The<br />
equinoxes drift westward along the ecliptic at the rate <strong>of</strong> 1 o<br />
per 72 years. This drift caused in the Julian Calendar a shifting<br />
<strong>of</strong> the dates for the equinox days.<br />
Indeed, since the Julian year is almost the same as the<br />
astronomical year, i.e. the time taken for the Earth to complete<br />
its orbit around the Sun, — the shifting <strong>of</strong> the spring<br />
equinox on the ecliptic results in shifting <strong>of</strong> the date <strong>of</strong> the<br />
spring equinox in Julian calendar (i.e. the “old style date”).<br />
In fact the “old style date” <strong>of</strong> the spring equinox, which in<br />
the Northern Hemisphere occurs now about March 21, is decreasing<br />
constantly at the rate <strong>of</strong> one day per 128 years (see<br />
Figure 4.7).<br />
In order to determine positions <strong>of</strong> celestial objects, we<br />
need a system <strong>of</strong> coordinates on the celestial sphere. There<br />
are several systems <strong>of</strong> coordinates used in astronomy, but we<br />
choose the so called system <strong>of</strong> ecliptic coordinates, which is<br />
illustrated on Figure 6.2. Consider a meridian on the celestial<br />
sphere from the pole P passing through the point A, for<br />
which we would like to determine its coordinates. The meridian<br />
intersects the ecliptic at the point D (see Figure 6.2). The<br />
length <strong>of</strong> the arc QD will be considered to be the ecliptic longitude<br />
<strong>of</strong> the point A, and the length <strong>of</strong> the arc AD — its<br />
ecliptic latitude (the both lengths measured in degrees). Let<br />
us recall that the point Q is the spring equinox point.<br />
In this way, the ecliptic longitude on the celestial sphere<br />
is calculated as a distance from the spring equinox point <strong>of</strong><br />
a specific epoch, which was chosen for this purpose. In other<br />
words, the system <strong>of</strong> ecliptic coordinates is “attached” to certain<br />
fixed epoch. However, once such an epoch is chosen, the<br />
related system <strong>of</strong> ecliptic coordinates can be used to describe<br />
the positions <strong>of</strong> the Sun, Moon, the planets, and, in fact, <strong>of</strong><br />
any celestial object at any moment <strong>of</strong> time from this or<br />
another epoch.<br />
In our calculations we used the ecliptic coordinate system<br />
attached to the ecliptic J2000, i.e. on January 1, 2000.<br />
We took, as the basis for the establishment <strong>of</strong> the ecliptic<br />
coordinates between the zodiacal constellations according to<br />
the ecliptic J2000, their J1900 coordinates (January 1, 1900) 6 .<br />
This partition <strong>of</strong> the ecliptic fits the contours <strong>of</strong> the constellations<br />
on an astronomical chart published in [49]. After readjusting<br />
this partition for the J2000 epoch (January 1, 2000),<br />
we obtained the results that are summarized in Table 6.1.<br />
We should explain that the boundaries <strong>of</strong> the constellations<br />
are not defined precisely on the sky. Therefore, any<br />
5 See [95].<br />
6 See [173], p. 782