Geography Reference
In-Depth Information
Here, we conclude with a representation of the left as well as the right inverse mapping, namely
Φ
−
l
:
}→
X
(
P,Q
)and
Φ
−
r
:
x
(
p, q
) in terms of conformal coordinates (isometric,
isothermal) of Box
1.37
, which specializes
Φ
−
l
and
Φ
−
r
of Box
1.21
.
{
P, Q
{
p, q
}→
End of Solution (the fourth problem).
Solution (the fifth problem).
By means of Fig.
1.27
, we illustrate why “UPS” is called
stereographic
. The stereographic projec-
tion of the “left” ellipsoid-of-revolution
r
isbaseduponthree
elements of
projective geometry
of type
central perspective
. First, we define the
perspective center
,
here the ellipsoidal “left” South Pole
S
l
as well as the spherical “right” South Pole
S
r
. Second, we
define the bundle of projection lines leaving
S
l
and
S
r
, respectively, and intersecting
A
1
,A
1
,A
2
E
and the “right” sphere
S
2
A
1
,A
1
,A
2
E
at
P
l
2
2
N
l
2
N
r
and
S
r
at
S
r
. Third, we define the projective plane
P
and
P
, respectively, namely the tangent
A
1
,A
1
,A
2
r
at the “right” spherical North
planes
T
N
l
E
at the “left” ellipsoidal North Pole and
T
N
r
S
Pole, respectively. The projection lines
S
l
→
P
l
intersect the projective plane at
p
l
,anelement
of the “left” tangent plane at the “left” North Pole, and the projection lines
S
r
P
r
intersect
the projective plane at
p
r
, an element of the “right” tangent plane at the “right” North Pole.
Note that we have collected th
e fundam
ental “left”
and “rig
ht” ratios of projective geometry in
→
Box
1.38
. Their conversion to
P
2
+
Q
2
“left” and
p
2
+
q
2
“right” generates the map
Φ
→
f
(
Φ
)
and
φ
→
g
(
φ
), respective
ly. The
projective planes are covered
by po
lar coord
inates
of type
{
P
2
+
Q
2
cos
α
l
,
P
2
+
Q
2
sin
α
l
}
{
p
2
+
q
2
cos
α
r
,
p
2
+
q
2
sin
α
r
}
“left”
and of type “right”
,
P
2
+
Q
2
,
p
2
+
q
2
respectively.
{
}
are the
radial coordinates
,
{
α
l
,α
r
}
are the “le
ft” and
“right”
South azimuths
. The central perspective generates
P
2
+
Q
2
=
f
(
Φ
)versus
p
2
+
q
2
=
g
(
φ
)
and
α
l
=
Λ
versus
α
r
=
λ
. Indeed, “UPS” is
azimuth preserving:
the “left” azimuth is identified
as ellipsoidal longitude, the “right” azimuth as spherical longitude, and
P
(
Λ, Φ
)=
f
(
Φ
)cos
Λ
versus
p
(
λ, φ
)=
g
(
Φ
)cos
λ,
(1.259)
Q
(
Λ, Φ
)=
f
(
Φ
)sin
Λ
versus
q
(
λ,
(
p
)=
g
(
Φ
)sin
λ.
End of Solution (the fifth problem).
Box 1.38 (Projective geometry of type central perspective).
Left projective ratio:
Right projective ratio:
S
l
N
l
,
√
X
2
+
Y
2
Z
l
P
l
N
l
p
l
=
S
l
Z
l
P
2
+
Q
2
=
A
2
+
Z
Z
r
P
r
N
r
p
r
=
S
r
Z
r
.
S
r
N
r
,
2
A
2
x
2
+
y
2
p
2
+
q
2
=
r
+
z
.
(1.260)
2
r
f
(
Φ
):
g
(
φ
):
A
1
cos
Φ
1
− E
2
sin
2
Φ
1
P
2
+
Q
2
=
r
cos
φ
p
2
+
q
2
=
Search WWH ::
Custom Search