Geography Reference
In-Depth Information
The construction principle is as follows. A point
P
0
(
L
0
,B
0
) is defined as the
origin
of a
local
reference system
.The
x
c
axis of the coordinate system, which is called “Hochwert” (Soldner
wording), agrees with the chosen
reference meridian L
0
. A point
P
(
L, B
) is described by
geodetic
parallel coordinates
as follows. Through the point
P
, we compute the
unique geodetic line
,which
cuts the meridian
L
0
at a right angle to produce the
footprint point P
F
. The length of the geodesic
P
-
P
F
is chosen as the
y
c
coordinate, which is called “Rechtswert” (Soldner wording). The angle
which is in between the local meridian of the point
P and
the
geodetic parallel
through the point
P
is called
meridian convergence γ
=
A
PF
−π/
2. The angle
γ
is fixed as the northern part of the
meridian, lefthand-oriented positive. We always say that the azimuth of the coordinate line
y
c
=
const. is the angle
γ
. Most notable, the geodetic parallel
y
c
=const.is
not
a geodesic. Compare
with Fig.
20.4
.
The
y
c
lines produce the
geodesic field
. In contrast, the
geodetic parallels are the orthogonal trajectories d
s
2
=
E
(
x
c
,y
c
)d
x
c
+d
y
c
=d
x
2
+
G
(
x, y
)d
y
2
.
20-31 First Problem of Soldner Coordinates: Geodetic Parallel
Coordinates, Input
{
L
0
,
B
0
,
x
c
=
y,
y
c
=
x
}
Versus Output
{
L
,
B
,γ
(Meridian Convergence)
}
For the problem of given coordinates
{
L
0
,B
0
,x
c
=
y, y
c
=
x
}
and unknown coordinates
, we use the standard method of Legendre series
u
=
s
cos
α
0
P
and
v
=
s
sin
α
0
P
.
In Box
20.7
, the details are collected.
{
L, B, γ
}
Box 20.7 (The problem of given coordinates
{L
0
,B
0
,x
c
=
y, y
c
=
x}
and unknown
coordinates
{L, B, γ}
).
First, we rewrite (
20.73
)-(
20.75
)intermsof
u
=
s
cos
α
0
P
and
v
=
s
sin
α
0
P
and obtain
(the coecients [
μν
] are collected in Box
20.5
and have to be computed at the point
B
0
)
B
P
=
B
0
+ [01]
v
versus
L
P
=
L
0
+ [10]
u
versus
α
P
0
=
α
0
P
+ [10]
α
u
+[20]
u
2
+[11]
uv
+[11]
α
uv
+[02]
v
2
+[12]
uv
2
+[12]
α
uv
2
+[21]
u
2
v
+[30]
u
3
+[30]
α
u
3
+[03]
v
3
+[31]
u
3
v
+[31]
α
u
3
v
(20.112)
+[40]
u
4
+[13]
uv
3
+[13]
α
uv
3
+[22]
u
2
v
2
+
...
+
....
+[04]
v
4
+
...
First step: determine
L
F
,B
F
,α
F0
, starting point
P
0
,s
=
y
=
x
c
,x
=
y
c
=0
,α
F0
=
π/
2
given.
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