Therefore M = 4 sin² ½[beta] - H²/H^1, and h must be determined so as
to make H²:H´ a maximum. In any particular case this maximum can only
be ascertained by trial, that is to say, log H² - log H´ must be
calculated for certain equidistant values of h, and then the
particular value of h which corresponds to the required maximum can
be obtained by interpolation. Thus we find that if it be required to
make the best possible perspective representation of a hemisphere, the
values of h and k are h = 1.47 and k = 2.034; so that in this case
2.034 sin u
[rho] = ------------.
1.47 + cos u
For a map of Africa or South America, the limiting radius [beta] we
may take as 40°; then in this case
2.543 sin u
[rho] = -------------.
1.625 + cos u
For Asia, [beta] = 54, and the distance h of the point of sight in
this case is 1.61. Fig. 11 is a map of Asia having the meridians and
parallels laid down on this system.
[Illustration: FIG. 11.]
Fig. 12 is a perspective representation of more than a hemisphere, the
radius [beta] being 108°, and the distance h of the point of vision,
1.40.
[Illustration: FIG. 12.--Twilight Projection. Clarke's Perspective
Projection for a Spherical Radius of 108°.]
The co-ordinates xy of any point in this perspective may be expressed
in terms of latitude and longitude of the corresponding point on the
sphere in the following manner. The co-ordinates originating at the
centre take the central meridian for the axis of y and a line
perpendicular to it for the axis of x. Let the latitude of the point
G, which is to occupy the centre of the map, be [gamma]; if [phi],
[omega] be the latitude and longitude of any point P (the longitude
being reckoned from the meridian of G), u the distance PG, and [mu]
the azimuth of P at G, then the spherical triangle whose sides are 90°
- [gamma], 90° - [phi], and u gives these relations--
sin u sin [mu] = cos [phi] sin [omega],
sin u cos [mu] = cos [gamma] sin [phi] - sin [gamma] cos [phi] cos [omega],
cos u = sin [gamma] sin [phi] + cos [gamma] cos [phi] cos [omega].
Now x = [rho] sin [mu], y = [rho] cos [mu], that is,
x cos [phi] sin [omega]
--- = -------------------------------------------------------------,
k h + sin [gamma] sin [phi] + cos [gamma] cos [phi] cos [omega]
y cos [gamma] sin [phi] - sin [gamma] cos [phi] cos [omega]
--- = -------------------------------------------------------------,
k h + sin [gamma] sin [phi] + cos [gamma] cos [phi] cos [omega]
Public-domain text, read in full here on John Shaqi.
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