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The Sun

Our solar model is sketched in Figure 17. From a geocentric point of view, the sun, $S$, appears to execute a (counterclockwise) Keplerian orbit of major radius $a$, and eccentricity $e$, about the earth, $G$. As has already been mentioned, the circle traced out by the sun on the celestial sphere is known as the ecliptic circle. This circle is inclined at $23^\circ 26'$ to the celestial equator, which is the projection of the earth's equator onto the celestial sphere. Suppose that the angle subtended at the earth between the vernal equinox (i.e., the point at which the sun passes the celestial equator from south to north) and the sun's perigee (i.e., the point of closest approach to the earth) is $\varpi$. This angle is termed the longitude of the perigee, and is assumed to vary linearly with time:
\begin{displaymath}
\varpi = \varpi_0 + \varpi_1\,(t-t_0).
\end{displaymath} (79)

Figure 17: The apparent orbit of the sun about the earth. Here, $S$, $G$, $\Pi$, $A$, $\varpi$, $T$, $\lambda$, and $\Upsilon$ represent the sun, earth, perigee, apogee, longitude of the perigee, true anomaly, ecliptic longitude, and vernal equinox, respectively. View is from northern ecliptic pole. The sun orbits counterclockwise.
\begin{figure}
\epsfysize =3in
\centerline{\epsffile{fig3.eps}}
\end{figure}

The sun's ecliptic longitude is defined as the angle subtended at the earth between the sun and the vernal equinox. Hence, from Fig. 17,

\begin{displaymath}
\lambda = \varpi + T,
\end{displaymath} (80)

where $T$ is the true anomaly. By analogy, the mean longitude is written
\begin{displaymath}
\bar{\lambda} = \varpi + M,
\end{displaymath} (81)

where $M$ is the mean anomaly. It follows from Eq. (23) that
\begin{displaymath}
\lambda = \bar{\lambda} + q,
\end{displaymath} (82)

where
\begin{displaymath}
q = 2\,e\,\sin M + (5/4)\,e^2\,\sin\,2M,
\end{displaymath} (83)

is called the equation of center. Note that $\lambda$, $\bar{\lambda}$, $T$, and $M$ are usually written as angles in the range $0^\circ $ to $360^\circ$, whereas $q$ is generally written as an angle in the range $-180^\circ$ to $+180^\circ$.

The mean longitude increases uniformly with time (since both $\varpi$ and $M$ increase uniformly with time) as

\begin{displaymath}
\bar{\lambda} = \bar{\lambda}_0+ n\,(t -t_0),
\end{displaymath} (84)

where $\bar{\lambda}_0$ is termed the mean longitude at epoch, $n$ the rate of motion in mean longitude, and $t_0$ the epoch. We can also write
\begin{displaymath}
M = M_0 + \tilde{n}\,(t-t_0),
\end{displaymath} (85)

where
\begin{displaymath}
M_0 = \bar{\lambda}_0 - \varpi_0
\end{displaymath} (86)

is called the mean anomaly at epoch, and
\begin{displaymath}
\tilde{n} = n - \varpi_1
\end{displaymath} (87)

the rate of motion in mean anomaly.

Our procedure for determining the ecliptic longitude of the sun is described below. The requisite orbital elements (i.e., $e$, $n$, $\tilde{n}$, $\bar{\lambda}_0$, and $M_0$) for the J2000 epoch (i.e., 12:00 GMT on January 1, 2000 CE, which corresponds to $t_0= 2\,451\,545.0$ JD) are listed in Table 30. These elements are calculated on the assumption that the vernal equinox precesses at the uniform rate of $-3.8246\times 10^{-5}\,\,^\circ/{\rm day}$. The ecliptic longitude of the sun is specified by the following formulae:

$\displaystyle \bar{\lambda}$ $\textstyle =$ $\displaystyle \bar{\lambda}_0+ n\,(t-t_0),$ (88)
$\displaystyle M$ $\textstyle =$ $\displaystyle M_0 + \tilde{n}\,(t-t_0),$ (89)
$\displaystyle q$ $\textstyle =$ $\displaystyle 2\,e\,\sin M + (5/4)\,e^2\,\sin\,2M,$ (90)
$\displaystyle \lambda$ $\textstyle =$ $\displaystyle \bar{\lambda} + q.$ (91)

These formulae are capable of matching NASA ephemeris data during the years 1995-2006 CE (see http://ssd.jpl.nasa.gov/) with a mean error of $0.2'$ and a maximum error of $0.7'$.

The ecliptic longitude of the sun can be calculated with the aid of Tables 32 and 33. Table 32 allows the mean longitude, $\bar{\lambda}$, and mean anomaly, $M$, of the sun to be determined as functions of time. Table 33 specifies the equation of center, $q$, as a function of the mean anomaly.

The procedure for using the tables is as follows:

  1. Determine the fractional Julian day number, $t$, corresponding to the date and time at which the sun's ecliptic longitude is to be calculated with the aid of Tables 1-3. Form $\Delta t = t-t_0$, where $t_0= 2\,451\,545.0$ is the epoch.
  2. Enter Table 32 with the digit for each power of 10 in ${\Delta} t$ and take out the corresponding values of $\Delta\bar{\lambda}$ and $\Delta M$. If $\Delta t$ is negative then the corresponding values are also negative. The value of the mean longitude, $\bar{\lambda}$, is the sum of all the $\Delta\bar{\lambda}$ values plus the value of $\bar{\lambda}$ at the epoch. Likewise, the value of the mean anomaly, $M$, is the sum of all the $\Delta M$ values plus the value of $M$ at the epoch. Add as many multiples of $360^\circ$ to $\bar{\lambda}$ and $M$ as is required to make them both fall in the range $0^\circ $ to $360^\circ$. Round $M$ to the nearest degree.
  3. Enter Table 33 with the value of $M$ and take out the corresponding value of the equation of center, $q$, and the radial anomaly, $\zeta$. (The latter step is only necessary if the ecliptic longitude of the sun is to be used to determine that of a planet.) It is necessary to interpolate if $M$ is odd.
  4. The ecliptic longitude, $\lambda$, is the sum of the mean longitude, $\bar{\lambda}$, and the equation of center, $q$. If necessary, convert $\lambda$ into an angle in the range $0^\circ $ to $360^\circ$. The decimal fraction can be converted into arc minutes using Table 31. Round to the nearest arc minute.
Two examples of the use of this procedure are given below.

Example 1: May 5, 2005 CE, 00:00 GMT:
 
According to Tables 1-3, $t = 2\,453\,495.5$ JD. Hence, $t-t_0 = 2\,453\,495.5-2\,451\,545.0=1\,950.5$ JD. Making use of Table 32, we find:
$t$(JD) $ \bar{\lambda}(^\circ)$ $M(^\circ)$
+1000 $265.647$ $265.600$
+900 $167.083$ $167.040$
+50 $49.280$ $49.280$
+.5 $0.493$ $0.493$
Epoch $280.458$ $357.588$
$762.961$ $840.001$
Modulus $42.961$ $120.001$

Rounding the mean anomaly to the nearest degree, we obtain $M\simeq 120^\circ$. It follows from Table 33 that

\begin{displaymath}
q(120^\circ)= 1.641^\circ,
\end{displaymath}

so

\begin{displaymath}
\lambda =\bar{\lambda} + q =42.961+ 1.641=44.602\simeq 44^\circ36'.
\end{displaymath}

Here, we have converted the decimal fraction into arc minutes using Table 31, and then rounded the final result to the nearest arc minute.

Following the practice of the Ancient Greeks (and modern-day astrologers), we shall express ecliptic longitudes in terms of the signs of the zodiac, which are listed in Sect. 4.6. The ecliptic longitude $44^\circ36'$ is conventionally written 14TA36: i.e., $14^\circ36'$ into the sign of Taurus. Thus, we conclude that the position of the sun at 00:00 GMT on May 5, 2005 CE was 14TA36.

Example 2: December 25, 1800 CE, 00:00 GMT:
 
According to Tables 1-3, $t = 2\,378\,854.5$ JD. Hence, $ t-t_0 = 2\,378\,854.5-2\,451\,545.0=-72\,690.5$ JD. Making use of Table 32, we find:
$t$(JD) $ \bar{\lambda}(^\circ)$ $M(^\circ)$
-70,000 $-235.315$ $-232.017$
-2,000 $-171.295$ $-171.200$
-600 $-231.388$ $-231.360$
-90 $-88.708$ $-88.704$
-.5 $-0.493$ $-0.493$
Epoch $280.458$ $357.588$
$-446.741$ $-366.186$
Modulus $273.259$ $353.814$

We conclude that $M\simeq 354^\circ$. From Table 33,

\begin{displaymath}
q(354^\circ)= -0.204^\circ,
\end{displaymath}

so

\begin{displaymath}
\lambda =\bar{\lambda} + q = 273.259 - 0.204=273.055\simeq 273^\circ03'.
\end{displaymath}

Thus, the position of the sun at 00:00 GMT on December 25, 1800 CE was 3CP03.

We can also use Tables 32 and 33 to calculate the dates of the equinoxes and solstices, and, hence, the lengths of the seasons, in a given year. The vernal equinox (i.e., the point on the sun's apparent orbit at which it passes the celestial equator from south to north) corresponds to $\lambda = 0^\circ$, the summer solstice (i.e., the point at which the sun is furthest north of the celestial equator) to $\lambda = 90^\circ$, the autumnal equinox (i.e., the point at which the sun passes the celestial equator from north to south) to $\lambda = 180^\circ$, and the winter solstice (i.e., the point at which the sun is furthest south of the celestial equator) to $\lambda = 270^\circ$--see Fig. 18. Furthermore, spring is defined as the period between the spring equinox and the summer solstice, summer as the period between the summer solstice and the autumnal equinox, autumn as the period between the autumnal equinox and the winter solstice, and winter as the period between the winter solstice and the following vernal equinox. Consider the year 2000 CE. For the case of the vernal equinox, we can first estimate the time at which this event takes place by approximating the solar longitude as the mean solar longitude: i.e.,

\begin{displaymath}
\lambda\simeq \bar{\lambda} = \bar{\lambda}_0 + n\,(t-t_0)
= 280.458 + 0.98564735\,(t-t_0),
\end{displaymath}

We obtain

\begin{displaymath}
t \simeq t_0+(360-280.458)/0.98564735 \simeq t_0+81\,{\rm JD}.
\end{displaymath}

Calculating the true solar longitude at this time, using Tables 32 and 33, we get $\lambda = 2.177^\circ.$ Now, the actual vernal equinox occurs when $\lambda = 0^\circ$. Thus, a much better estimate for the date of the vernal equinox is

\begin{displaymath}
t = t_0 + 81 -2.177/0.98564735 \simeq t_0 + 78.8\,{\rm JD},
\end{displaymath}

which corresponds to 7:00 GMT on March 20. Similar calculations show that the summer solstice takes place at

\begin{displaymath}
t = t_0+ 171.6\, {\rm JD},
\end{displaymath}

corresponding to 2:00 GMT on June 21, that the autumnal equinox takes place at

\begin{displaymath}
t = t_0+265.2\,{\rm JD},
\end{displaymath}

corresponding to 17:00 GMT on September 22, and that the winter solstice takes place at

\begin{displaymath}
t =t_0+355.1\, {\rm JD},
\end{displaymath}

corresponding to 14:00 GMT on December 21. Thus, the length of spring is $92.8$ days, the length of summer $93.6$ days, and the length of autumn $89.9$ days. Finally, the length of winter is the length of the tropical year (i.e., the time period between successive vernal equinoxes), which is $360/0.98564735 = 325.24$ days, minus the sum of the lengths of the other three seasons. This gives $88.9$ days.

Figure 18 illustrates the relationship between the equinox and solstice points, and the lengths of the seasons. The earth is displaced from the geometric center of the sun's apparent orbit in the direction of the perigee, which presently lies between the winter solstice and the vernal equinox. This displacement (which is greatly exaggerated in the figure) has two effects. Firstly, it causes the arc of the sun's apparent orbit between the summer solstice and autumnal equinox to be longer than that between the winter solstice and the vernal equinox. Secondly, it causes the sun to appear to move faster in winter than in summer, in accordance with Kepler's second law, since the sun is closer to the earth in the former season. Both of these effects tend to lengthen summer, and shorten winter. Hence, summer is presently the longest season, and winter the shortest.

At any particular observation site on the earth's surface, local noon is defined as the instant in time when the sun culminates at the meridian. However, as a consequence of the inclination of the ecliptic to the celestial equatior, as well as the uneven motion of the sun around the ecliptic, the time interval between successive local noons, which is known as a solar day, is not constant, but varies throughout the year. Hence, if we were to define a second as $1/86,400$ of a solar day then the length of a second would also vary throughout the year, which is clearly undesirable. In order to avoid this problem, astronomers have invented a fictitious body called the mean sun. The mean sun travels around the celestial equator (from west to east) at a constant rate which is such that it completes one orbit every tropical year. Local mean noon at a particular observation site is defined as the instance in time when the mean sun culminates at the meridian. Since the orbit of the mean sun is not inclined to the celestial equator, and the mean sun travels around the celestial equator at a uniform rate, the time interval between successive mean noons, which is known as a mean solar day, takes the constant value of 24 hours, or 86,400 seconds, throughout the year. Greenwich mean time (GMT) is defined such that 12:00 hrs. GMT coincides with mean noon every day at an observation site of terrestrial longitude $0^\circ $. If we define local mean time (LMT) as $LMT = GMT- \phi(^\circ)/15^\circ$ hrs., where $\phi$ is the terrestrial longitude of the observation site, then 12:00 hrs. LMT coincides with mean noon every day at a general observation site on the earth's surface.

According to the above definition, the right ascension, $\bar{\alpha}$, of the mean sun satisfies

\begin{displaymath}
\bar{\alpha} = \bar{\lambda},
\end{displaymath} (92)

where $\bar{\lambda}$ is the sun's mean ecliptic longitude. Moreover, it follows from Eqs. (41) and (82) that the right ascension of the true sun is given by
\begin{displaymath}
\tan\alpha = \cos\epsilon\,\tan(\bar{\lambda}+q),
\end{displaymath} (93)

where $\epsilon$ is the inclination of the ecliptic to the celestial equator, $q(M)$ the sun's equation of center, and $M$ its mean anomaly. Now, neglecting the small time variation of the longitude of the sun's perigee [i.e., setting $\varpi_1=0$ in Eq. (79)], we can write [see Eqs. (84), (85), and (87), as well as Table. 30]
\begin{displaymath}
M = \bar{\lambda} + M_0-\bar{\lambda}_0 = \bar{\lambda} +77.213^\circ.
\end{displaymath} (94)

It follows that, to first order in the solar eccentricity, $e$, we have
\begin{displaymath}
\Delta\alpha = \bar{\alpha}-\alpha = \lambda - \tan^{-1}(\cos \epsilon\,\tan\lambda) - 2\,e\,\sin\,M,
\end{displaymath} (95)

where
\begin{displaymath}
M = \lambda + 77.213^\circ.
\end{displaymath} (96)

Now,
\begin{displaymath}
\Delta t({\rm hrs.}) = \Delta\alpha(^\circ)/15^\circ
\end{displaymath} (97)

represents the time difference between local noon and mean local noon (since right ascension crosses the meridian at the uniform rate of $15^\circ$ an hour), and is known as the equation of time. If $\Delta t$ is positive then local noon occurs before mean local noon, and vice versa.

The equation of time specifies the difference between time calculated using a sundial or sextant--which is known as solar time--and time obtained from an accurate clock--which is known as mean solar time. Table 34 shows the equation of time as a function of the sun's ecliptic longitude. It can be seen that the difference between solar time and mean solar time can be as much as 16 minutes, and attains its maximum value between the autumnal equinox and the winter solstice, and its minimum value between the winter solstice and vernal equinox.

Figure 18: The sun's apparent orbit around the earth, $G$, showing the vernal equinox (VE), summer solstice (SS), autumnal equinox (AE), and winter solstice (WS). Here, $\lambda$, $\Pi$, $A$, and $C$ are the ecliptic longitude, perigee, apogee, and geometric center of the orbit, respectively. The lengths of the seasons (in days) are indicated.
\begin{figure}
\epsfysize =3.5in
\centerline{\epsffile{solstice.eps}}
\end{figure}


Table 30: Keplerian orbital elements for the sun and the five visible planets at the J2000 epoch (i.e., 12:00 GMT, January 1, 2000 CE, which corresponds to $t_0= 2\,451\,545.0$ JD). The elements are optimized for use in the time period 1800 CE to 2050 CE. Source: Jet Propulsion Laboratory (NASA), http://ssd.jpl.nasa.gov/. The motion rates have been converted into tropical motion rates assuming a uniform precession of the equinoxes of $3.8246\times 10^{-5}\,\,^\circ/{\rm day}$.
Object $a\,(AU)$ $e$ $n\,(^\circ/{\rm day})$ $\tilde{n}\,(^\circ/{\rm day})$ $\bar{\lambda}_0\,(^\circ)$ $M_0\,(^\circ)$
             
Mercury $0.387098$ $0.205636$ $4.09237703$ $4.09233439$ $252.087$ $174.693$
Venus $0.723334$ $0.006777$ $1.60216872$ $1.60213040$ $181.973$ $49.237$
Sun $1.000000$ $0.016711$ $0.98564735$ $0.98560025$ $280.458$ $357.588$
Mars $1.523706$ $0.093394$ $0.52407118$ $0.52402076$ $355.460$ $19.388$
Jupiter $5.202873$ $0.048386$ $0.08312507$ $0.08308100$ $34.365$ $19.348$
Saturn $9.536651$ $0.053862$ $0.03350830$ $0.03348152$ $50.059$ $317.857$



Table 31: Arc minute to decimal fraction conversion table.
$00.0'$ .000 $10.0'$ .167 $20.0'$ .333 $30.0'$ .500 $40.0'$ .667 $50.0'$ .833
$00.2'$ .003 $10.2'$ .170 $20.2'$ .337 $30.2'$ .503 $40.2'$ .670 $50.2'$ .837
$00.4'$ .007 $10.4'$ .173 $20.4'$ .340 $30.4'$ .507 $40.4'$ .673 $50.4'$ .840
$00.6'$ .010 $10.6'$ .177 $20.6'$ .343 $30.6'$ .510 $40.6'$ .677 $50.6'$ .843
$00.8'$ .013 $10.8'$ .180 $20.8'$ .347 $30.8'$ .513 $40.8'$ .680 $50.8'$ .847
$01.0'$ .017 $11.0'$ .183 $21.0'$ .350 $31.0'$ .517 $41.0'$ .683 $51.0'$ .850
$01.2'$ .020 $11.2'$ .187 $21.2'$ .353 $31.2'$ .520 $41.2'$ .687 $51.2'$ .853
$01.4'$ .023 $11.4'$ .190 $21.4'$ .357 $31.4'$ .523 $41.4'$ .690 $51.4'$ .857
$01.6'$ .027 $11.6'$ .193 $21.6'$ .360 $31.6'$ .527 $41.6'$ .693 $51.6'$ .860
$01.8'$ .030 $11.8'$ .197 $21.8'$ .363 $31.8'$ .530 $41.8'$ .697 $51.8'$ .863
$02.0'$ .033 $12.0'$ .200 $22.0'$ .367 $32.0'$ .533 $42.0'$ .700 $52.0'$ .867
$02.2'$ .037 $12.2'$ .203 $22.2'$ .370 $32.2'$ .537 $42.2'$ .703 $52.2'$ .870
$02.4'$ .040 $12.4'$ .207 $22.4'$ .373 $32.4'$ .540 $42.4'$ .707 $52.4'$ .873
$02.6'$ .043 $12.6'$ .210 $22.6'$ .377 $32.6'$ .543 $42.6'$ .710 $52.6'$ .877
$02.8'$ .047 $12.8'$ .213 $22.8'$ .380 $32.8'$ .547 $42.8'$ .713 $52.8'$ .880
$03.0'$ .050 $13.0'$ .217 $23.0'$ .383 $33.0'$ .550 $43.0'$ .717 $53.0'$ .883
$03.2'$ .053 $13.2'$ .220 $23.2'$ .387 $33.2'$ .553 $43.2'$ .720 $53.2'$ .887
$03.4'$ .057 $13.4'$ .223 $23.4'$ .390 $33.4'$ .557 $43.4'$ .723 $53.4'$ .890
$03.6'$ .060 $13.6'$ .227 $23.6'$ .393 $33.6'$ .560 $43.6'$ .727 $53.6'$ .893
$03.8'$ .063 $13.8'$ .230 $23.8'$ .397 $33.8'$ .563 $43.8'$ .730 $53.8'$ .897
$04.0'$ .067 $14.0'$ .233 $24.0'$ .400 $34.0'$ .567 $44.0'$ .733 $54.0'$ .900
$04.2'$ .070 $14.2'$ .237 $24.2'$ .403 $34.2'$ .570 $44.2'$ .737 $54.2'$ .903
$04.4'$ .073 $14.4'$ .240 $24.4'$ .407 $34.4'$ .573 $44.4'$ .740 $54.4'$ .907
$04.6'$ .077 $14.6'$ .243 $24.6'$ .410 $34.6'$ .577 $44.6'$ .743 $54.6'$ .910
$04.8'$ .080 $14.8'$ .247 $24.8'$ .413 $34.8'$ .580 $44.8'$ .747 $54.8'$ .913
$05.0'$ .083 $15.0'$ .250 $25.0'$ .417 $35.0'$ .583 $45.0'$ .750 $55.0'$ .917
$05.2'$ .087 $15.2'$ .253 $25.2'$ .420 $35.2'$ .587 $45.2'$ .753 $55.2'$ .920
$05.4'$ .090 $15.4'$ .257 $25.4'$ .423 $35.4'$ .590 $45.4'$ .757 $55.4'$ .923
$05.6'$ .093 $15.6'$ .260 $25.6'$ .427 $35.6'$ .593 $45.6'$ .760 $55.6'$ .927
$05.8'$ .097 $15.8'$ .263 $25.8'$ .430 $35.8'$ .597 $45.8'$ .763 $55.8'$ .930
$06.0'$ .100 $16.0'$ .267 $26.0'$ .433 $36.0'$ .600 $46.0'$ .767 $56.0'$ .933
$06.2'$ .103 $16.2'$ .270 $26.2'$ .437 $36.2'$ .603 $46.2'$ .770 $56.2'$ .937
$06.4'$ .107 $16.4'$ .273 $26.4'$ .440 $36.4'$ .607 $46.4'$ .773 $56.4'$ .940
$06.6'$ .110 $16.6'$ .277 $26.6'$ .443 $36.6'$ .610 $46.6'$ .777 $56.6'$ .943
$06.8'$ .113 $16.8'$ .280 $26.8'$ .447 $36.8'$ .613 $46.8'$ .780 $56.8'$ .947
$07.0'$ .117 $17.0'$ .283 $27.0'$ .450 $37.0'$ .617 $47.0'$ .783 $57.0'$ .950
$07.2'$ .120 $17.2'$ .287 $27.2'$ .453 $37.2'$ .620 $47.2'$ .787 $57.2'$ .953
$07.4'$ .123 $17.4'$ .290 $27.4'$ .457 $37.4'$ .623 $47.4'$ .790 $57.4'$ .957
$07.6'$ .127 $17.6'$ .293 $27.6'$ .460 $37.6'$ .627 $47.6'$ .793 $57.6'$ .960
$07.8'$ .130 $17.8'$ .297 $27.8'$ .463 $37.8'$ .630 $47.8'$ .797 $57.8'$ .963
$08.0'$ .133 $18.0'$ .300 $28.0'$ .467 $38.0'$ .633 $48.0'$ .800 $58.0'$ .967
$08.2'$ .137 $18.2'$ .303 $28.2'$ .470 $38.2'$ .637 $48.2'$ .803 $58.2'$ .970
$08.4'$ .140 $18.4'$ .307 $28.4'$ .473 $38.4'$ .640 $48.4'$ .807 $58.4'$ .973
$08.6'$ .143 $18.6'$ .310 $28.6'$ .477 $38.6'$ .643 $48.6'$ .810 $58.6'$ .977
$08.8'$ .147 $18.8'$ .313 $28.8'$ .480 $38.8'$ .647 $48.8'$ .813 $58.8'$ .980
$09.0'$ .150 $19.0'$ .317 $29.0'$ .483 $39.0'$ .650 $49.0'$ .817 $59.0'$ .983
$09.2'$ .153 $19.2'$ .320 $29.2'$ .487 $39.2'$ .653 $49.2'$ .820 $59.2'$ .987
$09.4'$ .157 $19.4'$ .323 $29.4'$ .490 $39.4'$ .657 $49.4'$ .823 $59.4'$ .990
$09.6'$ .160 $19.6'$ .327 $29.6'$ .493 $39.6'$ .660 $49.6'$ .827 $59.6'$ .993
$09.8'$ .163 $19.8'$ .330 $29.8'$ .497 $39.8'$ .663 $49.8'$ .830 $59.8'$ .997



Table 32: Mean motion of the sun. Here, $\Delta t = t-t_0$, $\Delta\bar{\lambda} = \bar{\lambda}-\bar{\lambda}_0$, and $\Delta M = M - M_0$. At epoch ( $t_0= 2\,451\,545.0$ JD), $\bar{\lambda}_0 = 280.458^\circ$, and $M_0 = 357.588^\circ$.
$\Delta t$(JD) $\Delta\bar{\lambda}(^\circ)$ $\Delta M(^\circ)$ $\Delta t$(JD) $\Delta\bar{\lambda}(^\circ)$ $\Delta M(^\circ)$ $\Delta t$(JD) $\Delta\bar{\lambda}(^\circ)$ $\Delta M(^\circ)$
                 
10,000 136.474 136.002 1,000 265.647 265.600 100 98.565 98.560
20,000 272.947 272.005 2,000 171.295 171.200 200 197.129 197.120
30,000 49.421 48.007 3,000 76.942 76.801 300 295.694 295.680
40,000 185.894 184.010 4,000 342.589 342.401 400 34.259 34.240
50,000 322.367 320.012 5,000 248.237 248.001 500 132.824 132.800
60,000 98.841 96.015 6,000 153.884 153.601 600 231.388 231.360
70,000 235.315 232.017 7,000 59.531 59.202 700 329.953 329.920
80,000 11.788 8.020 8,000 325.179 324.802 800 68.518 68.480
90,000 148.262 144.022 9,000 230.826 230.402 900 167.083 167.040
                 
10 9.856 9.856 1 0.986 0.986 0.1 0.099 0.099
20 19.713 19.712 2 1.971 1.971 0.2 0.197 0.197
30 29.569 29.568 3 2.957 2.957 0.3 0.296 0.296
40 39.426 39.424 4 3.943 3.942 0.4 0.394 0.394
50 49.282 49.280 5 4.928 4.928 0.5 0.493 0.493
60 59.139 59.136 6 5.914 5.914 0.6 0.591 0.591
70 68.995 68.992 7 6.900 6.899 0.7 0.690 0.690
80 78.852 78.848 8 7.885 7.885 0.8 0.789 0.788
90 88.708 88.704 9 8.871 8.870 0.9 0.887 0.887



Table 33: Anomalies of the sun.
$M(^\circ)$ $q(^\circ)$ $100\,\zeta$ $M(^\circ)$ $q(^\circ)$ $100\,\zeta$ $M(^\circ)$ $q(^\circ)$ $100\,\zeta$ $M(^\circ)$ $q(^\circ)$ $100\,\zeta$
0 0.000 1.671 90 1.915 -0.028 180 0.000 -1.671 270 -1.915 -0.028
2 0.068 1.670 92 1.912 -0.086 182 -0.065 -1.670 272 -1.915 0.030
4 0.136 1.667 94 1.907 -0.144 184 -0.131 -1.667 274 -1.913 0.089
6 0.204 1.662 96 1.900 -0.202 186 -0.196 -1.662 276 -1.909 0.147
8 0.272 1.654 98 1.891 -0.260 188 -0.261 -1.655 278 -1.902 0.205
10 0.339 1.645 100 1.879 -0.317 190 -0.326 -1.647 280 -1.893 0.263
12 0.406 1.633 102 1.865 -0.374 192 -0.390 -1.636 282 -1.881 0.321
14 0.473 1.620 104 1.849 -0.431 194 -0.454 -1.623 284 -1.867 0.378
16 0.538 1.604 106 1.830 -0.486 196 -0.517 -1.608 286 -1.851 0.435
18 0.604 1.587 108 1.809 -0.542 198 -0.580 -1.592 288 -1.833 0.491
20 0.668 1.567 110 1.787 -0.596 200 -0.642 -1.574 290 -1.812 0.547
22 0.731 1.545 112 1.762 -0.650 202 -0.703 -1.553 292 -1.789 0.602
24 0.794 1.522 114 1.735 -0.703 204 -0.764 -1.531 294 -1.764 0.656
26 0.855 1.497 116 1.705 -0.755 206 -0.824 -1.507 296 -1.737 0.710
28 0.916 1.469 118 1.674 -0.806 208 -0.882 -1.482 298 -1.707 0.763
30 0.975 1.440 120 1.641 -0.856 210 -0.940 -1.454 300 -1.676 0.815
32 1.033 1.409 122 1.606 -0.906 212 -0.997 -1.425 302 -1.642 0.865
34 1.089 1.377 124 1.569 -0.954 214 -1.052 -1.394 304 -1.606 0.915
36 1.145 1.342 126 1.530 -1.001 216 -1.107 -1.362 306 -1.568 0.964
38 1.198 1.306 128 1.490 -1.046 218 -1.160 -1.327 308 -1.528 1.011
40 1.251 1.269 130 1.447 -1.091 220 -1.211 -1.292 310 -1.487 1.058
42 1.301 1.229 132 1.403 -1.134 222 -1.261 -1.254 312 -1.443 1.103
44 1.350 1.189 134 1.358 -1.175 224 -1.310 -1.216 314 -1.397 1.146
46 1.397 1.146 136 1.310 -1.216 226 -1.358 -1.175 316 -1.350 1.189
48 1.443 1.103 138 1.261 -1.254 228 -1.403 -1.134 318 -1.301 1.229
50 1.487 1.058 140 1.211 -1.292 230 -1.447 -1.091 320 -1.251 1.269
52 1.528 1.011 142 1.160 -1.327 232 -1.490 -1.046 322 -1.198 1.306
54 1.568 0.964 144 1.107 -1.362 234 -1.530 -1.001 324 -1.145 1.342
56 1.606 0.915 146 1.052 -1.394 236 -1.569 -0.954 326 -1.089 1.377
58 1.642 0.865 148 0.997 -1.425 238 -1.606 -0.906 328 -1.033 1.409
60 1.676 0.815 150 0.940 -1.454 240 -1.641 -0.856 330 -0.975 1.440
62 1.707 0.763 152 0.882 -1.482 242 -1.674 -0.806 332 -0.916 1.469
64 1.737 0.710 154 0.824 -1.507 244 -1.705 -0.755 334 -0.855 1.497
66 1.764 0.656 156 0.764 -1.531 246 -1.735 -0.703 336 -0.794 1.522
68 1.789 0.602 158 0.703 -1.553 248 -1.762 -0.650 338 -0.731 1.545
70 1.812 0.547 160 0.642 -1.574 250 -1.787 -0.596 340 -0.668 1.567
72 1.833 0.491 162 0.580 -1.592 252 -1.809 -0.542 342 -0.604 1.587
74 1.851 0.435 164 0.517 -1.608 254 -1.830 -0.486 344 -0.538 1.604
76 1.867 0.378 166 0.454 -1.623 256 -1.849 -0.431 346 -0.473 1.620
78 1.881 0.321 168 0.390 -1.636 258 -1.865 -0.374 348 -0.406 1.633
80 1.893 0.263 170 0.326 -1.647 260 -1.879 -0.317 350 -0.339 1.645
82 1.902 0.205 172 0.261 -1.655 262 -1.891 -0.260 352 -0.272 1.654
84 1.909 0.147 174 0.196 -1.662 264 -1.900 -0.202 354 -0.204 1.662
86 1.913 0.089 176 0.131 -1.667 266 -1.907 -0.144 356 -0.136 1.667
88 1.915 0.030 178 0.065 -1.670 268 -1.912 -0.086 358 -0.068 1.670
90 1.915 -0.028 180 0.000 -1.671 270 -1.915 -0.028 360 -0.000 1.671



Table 34: The equation of time. The superscripts $m$ and $s$ denote minutes and seconds.
Aries Taurus Gemini Cancer Leo Virgo
$\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$
00$^\circ$ -07$^m$28$^s$ 00$^\circ$ +01$^m$02$^s$ 00$^\circ$ +03$^m$30$^s$ 00$^\circ$ -01$^m$42$^s$ 00$^\circ$ -06$^m$27$^s$ 00$^\circ$ -02$^m$44$^s$
02$^\circ$ -06$^m$51$^s$ 02$^\circ$ +01$^m$27$^s$ 02$^\circ$ +03$^m$21$^s$ 02$^\circ$ -02$^m$09$^s$ 02$^\circ$ -06$^m$30$^s$ 02$^\circ$ -02$^m$11$^s$
04$^\circ$ -06$^m$15$^s$ 04$^\circ$ +01$^m$50$^s$ 04$^\circ$ +03$^m$10$^s$ 04$^\circ$ -02$^m$36$^s$ 04$^\circ$ -06$^m$31$^s$ 04$^\circ$ -01$^m$36$^s$
06$^\circ$ -05$^m$38$^s$ 06$^\circ$ +02$^m$12$^s$ 06$^\circ$ +02$^m$56$^s$ 06$^\circ$ -03$^m$03$^s$ 06$^\circ$ -06$^m$29$^s$ 06$^\circ$ +00$^m$59$^s$
08$^\circ$ -05$^m$01$^s$ 08$^\circ$ +02$^m$31$^s$ 08$^\circ$ +02$^m$41$^s$ 08$^\circ$ -03$^m$29$^s$ 08$^\circ$ -06$^m$24$^s$ 08$^\circ$ +00$^m$21$^s$
10$^\circ$ -04$^m$24$^s$ 10$^\circ$ +02$^m$48$^s$ 10$^\circ$ +02$^m$23$^s$ 10$^\circ$ -03$^m$53$^s$ 10$^\circ$ -06$^m$16$^s$ 10$^\circ$ +00$^m$18$^s$
12$^\circ$ -03$^m$48$^s$ 12$^\circ$ +03$^m$03$^s$ 12$^\circ$ +02$^m$04$^s$ 12$^\circ$ -04$^m$17$^s$ 12$^\circ$ -06$^m$06$^s$ 12$^\circ$ +00$^m$58$^s$
14$^\circ$ -03$^m$12$^s$ 14$^\circ$ +03$^m$16$^s$ 14$^\circ$ +01$^m$43$^s$ 14$^\circ$ -04$^m$39$^s$ 14$^\circ$ -05$^m$54$^s$ 14$^\circ$ +01$^m$40$^s$
16$^\circ$ -02$^m$36$^s$ 16$^\circ$ +03$^m$26$^s$ 16$^\circ$ +01$^m$20$^s$ 16$^\circ$ -05$^m$00$^s$ 16$^\circ$ -05$^m$38$^s$ 16$^\circ$ +02$^m$22$^s$
18$^\circ$ -02$^m$01$^s$ 18$^\circ$ +03$^m$34$^s$ 18$^\circ$ +00$^m$57$^s$ 18$^\circ$ -05$^m$19$^s$ 18$^\circ$ -05$^m$20$^s$ 18$^\circ$ +03$^m$05$^s$
20$^\circ$ -01$^m$28$^s$ 20$^\circ$ +03$^m$40$^s$ 20$^\circ$ +00$^m$32$^s$ 20$^\circ$ -05$^m$35$^s$ 20$^\circ$ -05$^m$00$^s$ 20$^\circ$ +03$^m$49$^s$
22$^\circ$ +00$^m$55$^s$ 22$^\circ$ +03$^m$43$^s$ 22$^\circ$ +00$^m$06$^s$ 22$^\circ$ -05$^m$50$^s$ 22$^\circ$ -04$^m$37$^s$ 22$^\circ$ +04$^m$32$^s$
24$^\circ$ +00$^m$23$^s$ 24$^\circ$ +03$^m$43$^s$ 24$^\circ$ +00$^m$20$^s$ 24$^\circ$ -06$^m$03$^s$ 24$^\circ$ -04$^m$12$^s$ 24$^\circ$ +05$^m$16$^s$
26$^\circ$ +00$^m$06$^s$ 26$^\circ$ +03$^m$41$^s$ 26$^\circ$ +00$^m$47$^s$ 26$^\circ$ -06$^m$14$^s$ 26$^\circ$ -03$^m$45$^s$ 26$^\circ$ +06$^m$00$^s$
28$^\circ$ +00$^m$34$^s$ 28$^\circ$ +03$^m$37$^s$ 28$^\circ$ -01$^m$14$^s$ 28$^\circ$ -06$^m$22$^s$ 28$^\circ$ -03$^m$15$^s$ 28$^\circ$ +06$^m$44$^s$
30$^\circ$ +01$^m$02$^s$ 30$^\circ$ +03$^m$30$^s$ 30$^\circ$ -01$^m$42$^s$ 30$^\circ$ -06$^m$27$^s$ 30$^\circ$ -02$^m$44$^s$ 30$^\circ$ +07$^m$28$^s$
Libra Scorpio Sagittarius Capricorn Aquarius Pisces
$\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$ $\lambda$ $\Delta t~~~~~$
00$^\circ$ +07$^m$28$^s$ 00$^\circ$ +15$^m$40$^s$ 00$^\circ$ +13$^m$55$^s$ 00$^\circ$ +01$^m$42$^s$ 00$^\circ$ -10$^m$58$^s$ 00$^\circ$ -13$^m$58$^s$
02$^\circ$ +08$^m$10$^s$ 02$^\circ$ +15$^m$55$^s$ 02$^\circ$ +13$^m$22$^s$ 02$^\circ$ +00$^m$43$^s$ 02$^\circ$ -11$^m$32$^s$ 02$^\circ$ -13$^m$46$^s$
04$^\circ$ +08$^m$53$^s$ 04$^\circ$ +16$^m$08$^s$ 04$^\circ$ +12$^m$46$^s$ 04$^\circ$ +00$^m$15$^s$ 04$^\circ$ -12$^m$02$^s$ 04$^\circ$ -13$^m$31$^s$
06$^\circ$ +09$^m$34$^s$ 06$^\circ$ +16$^m$17$^s$ 06$^\circ$ +12$^m$08$^s$ 06$^\circ$ -01$^m$13$^s$ 06$^\circ$ -12$^m$30$^s$ 06$^\circ$ -13$^m$14$^s$
08$^\circ$ +10$^m$14$^s$ 08$^\circ$ +16$^m$23$^s$ 08$^\circ$ +11$^m$26$^s$ 08$^\circ$ -02$^m$11$^s$ 08$^\circ$ -12$^m$54$^s$ 08$^\circ$ -12$^m$55$^s$
10$^\circ$ +10$^m$53$^s$ 10$^\circ$ +16$^m$26$^s$ 10$^\circ$ +10$^m$42$^s$ 10$^\circ$ -03$^m$07$^s$ 10$^\circ$ -13$^m$16$^s$ 10$^\circ$ -12$^m$33$^s$
12$^\circ$ +11$^m$30$^s$ 12$^\circ$ +16$^m$26$^s$ 12$^\circ$ +09$^m$55$^s$ 12$^\circ$ -04$^m$03$^s$ 12$^\circ$ -13$^m$34$^s$ 12$^\circ$ -12$^m$10$^s$
14$^\circ$ +12$^m$06$^s$ 14$^\circ$ +16$^m$23$^s$ 14$^\circ$ +09$^m$07$^s$ 14$^\circ$ -04$^m$57$^s$ 14$^\circ$ -13$^m$49$^s$ 14$^\circ$ -11$^m$44$^s$
16$^\circ$ +12$^m$41$^s$ 16$^\circ$ +16$^m$16$^s$ 16$^\circ$ +08$^m$16$^s$ 16$^\circ$ -05$^m$50$^s$ 16$^\circ$ -14$^m$01$^s$ 16$^\circ$ -11$^m$17$^s$
18$^\circ$ +13$^m$13$^s$ 18$^\circ$ +16$^m$06$^s$ 18$^\circ$ +07$^m$23$^s$ 18$^\circ$ -06$^m$41$^s$ 18$^\circ$ -14$^m$09$^s$ 18$^\circ$ -10$^m$48$^s$
20$^\circ$ +13$^m$43$^s$ 20$^\circ$ +15$^m$52$^s$ 20$^\circ$ +06$^m$29$^s$ 20$^\circ$ -07$^m$30$^s$ 20$^\circ$ -14$^m$15$^s$ 20$^\circ$ -10$^m$17$^s$
22$^\circ$ +14$^m$12$^s$ 22$^\circ$ +15$^m$36$^s$ 22$^\circ$ +05$^m$33$^s$ 22$^\circ$ -08$^m$16$^s$ 22$^\circ$ -14$^m$17$^s$ 22$^\circ$ -09$^m$45$^s$
24$^\circ$ +14$^m$38$^s$ 24$^\circ$ +15$^m$15$^s$ 24$^\circ$ +04$^m$37$^s$ 24$^\circ$ -09$^m$01$^s$ 24$^\circ$ -14$^m$17$^s$ 24$^\circ$ -09$^m$12$^s$
26$^\circ$ +15$^m$01$^s$ 26$^\circ$ +14$^m$52$^s$ 26$^\circ$ +03$^m$39$^s$ 26$^\circ$ -09$^m$42$^s$ 26$^\circ$ -14$^m$13$^s$ 26$^\circ$ -08$^m$38$^s$
28$^\circ$ +15$^m$22$^s$ 28$^\circ$ +14$^m$25$^s$ 28$^\circ$ +02$^m$41$^s$ 28$^\circ$ -10$^m$22$^s$ 28$^\circ$ -14$^m$07$^s$ 28$^\circ$ -08$^m$03$^s$
30$^\circ$ +15$^m$40$^s$ 30$^\circ$ +13$^m$55$^s$ 30$^\circ$ +01$^m$42$^s$ 30$^\circ$ -10$^m$58$^s$ 30$^\circ$ -13$^m$58$^s$ 30$^\circ$ -07$^m$28$^s$



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Next: The Moon Up: Almagest Previous: Ecliptic Altitude and Orientation
Richard Fitzpatrick 2008-02-25