point. Azimuth is measured in degrees from 0° to 360°.
The conventional symbol for azimuth is the letter A or
Z.
Astronomical Triangle
The solutions of problems involving the three
coordinate systems are made by means of spherical
trigonometry. A figure of prime importance is the
spherical triangle that lies on the celestial sphere and
whose vertices are the pole, the zenith, and the
celestial body involved. This is known as the
astronomical or the PZS (pole-zenith-star) triangle.
The astronomical triangle is shown in figure 15-3.
As in the case of all spherical triangles, the sides can
be expressed as the angles subtended at the center of
the sphere. In the astronomical triangle, the side
between the pole and the zenith is the colatitude
(90° - 0), between the pole and the star is the
codeclination or polar distance (90° - 6), and between
the zenith and the star is the coaltitude, or zenith
distance (90° - h). The angle at the zenith is the
azimuth angle (A) of the body. The angle at the pole
is the hour angle (t). The angle at the star is known as
the parallactic angle and is little used in computa-
tions. If the three elements of the astronomic triangle
are known, the others can be found by means of spheri-
cal trigonometry. The fundamental equation is the law
of cosines. cos a = cos b cos c + sin b sin c cos a, in
which a, b, and c are the sides of a spherical triangle,
and A is the angle opposite side a (B and C are the
angles opposite sides b and c, respectively). All
formulas required for the solution of the astronomic
triangle may be derived from this law of cosines.
Astronomical Tables
Used by Surveyors
The declination and Greenwich hour angle of the
sun, moon, and selected planets are given for every even
hour of GMT for everyday in the year in the daily pages
of the Nautical Almanac and the Ephemeris of the Sun,
Polaris, and Other Selected Stars. These publications
are prepared by the U.S. Naval Observatory and are
available for sale at the U.S. Government Printing
Office, Washington, D.C. Condensed tables of data are
also available from various manufacturers of surveying
equipment.
Suppose that you want to determine the GHA and
declination of the sun for an observation made at zone
time l&23m18 on 17 May 1986 in longitude
793712W. The ZD is +5; therefore, GMT Of the
observation was 15~23m18.
Table 15-1 shows the relevant daily page of the 1986
Nautical Almanac. You can see that for 15~~O& on 17
May the GHA listed for the sun is 45054.8. For the extra
2318S you turn to a table of increments and
corrections in the back of the book. Table 15-2 shows
the relevant page of the table. Under 23m and beside 18s
in the Sun column you find an increment of 5049.5. The
GHA of the sun at the time of observation, then, was
45°54.8 + 5049.5, or 51044.3.
On the daily page of 17 May (table 15-1), the
Nautical Almanac gives a sun declination for 15%000
GMT on N 19°21.3. At the foot of the column, you
see a small d and the figure 0.6. In the increments and
corrections table (table 15-2), you see a column of v
or d corrections for declination. You go down this
column to the figure 0.6, where you find that the d
correction in this case is 0.2'. Whether you add this
correction or subtract it depends upon whether the
declination of the sun is increasing or decreasing with
time. A glance at the daily page shows that in this case,
it is increasing; therefore, the declination of the sun at
the time of observation was N 19°21.3 + 0.2, or
N 19021.5.
On an opposing daily page of the Nautical Almanac
(table 5-3), the declinations of a select list of 57
prominent stars are given. Instead of the GHAs of these
stars, however, the sidereal hour angle (SHA) of each
star is given. The sidereal angle of a star is its arc
distance westward from the vernal equinox or first point
of Aries. The GHA of a star is its arc distance westward
from the hour circle of the first point of Aries.
For GHA of a star, you first determine GHA of the
first point of Aries in the same manner described for the
sun. You can see Aries listed in tables 15-2 and 15-3.
You then add this to the SHA of the star, as given in the
daily page of the Nautical Almanac (table 15-3). This
can be stated as follows: GHA star= GHA Aries + SHA
star. If the result is greater than 360°, you subtract 360°
from it.
For declination of a star, you use the declination
listed on the daily page; this is good for a star at anytime
of the day.
NOTE: The SHA and GHA of the vernal equinox
are factors used in star observations; however, neither is
applicable in observation of navigational plaints.
15-7