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Thus, it can be seen that with y
ᄐ
0 and
Δ
S
ᄐ
0, the distance correction on the
central meridian is zero. In the case of y
0, we see that the distance
correction is always a positive value, increasing with the distance from the central
meridian. When y
m
ᄐ
6ᄐ
0 and
Δ
S
>
300 km, S
ᄐ
5 km, and R
m
ᄐ
6, 400 km, we can get
Δ
S
ᄐ
6 m after
the distance correction. Obviously,
the distance correction is
non-negligible in computations of all orders.
Also, if converting the planar chord-length D to the geodesic distance S,we
have:
S
ᄐ
D
Δ
S
ð
6
:
75
Þ
Accuracy of Coordinates Required in the Computation of Distance
Correction
To calculate the distance correction one needs to know the plane coordinates of a
point. As the value of the distance correction is not large, it does not require too
high a level of coordinate accuracy. To know the approximations of coordinates is
sufficient; we will analyze the desired degree of accuracy for coordinates.
From (
6.74
), we get:
2y
m
Δ
ð
D
S
Þᄐ
2R
m
2
S
Δ
y
and
R
m
2
y
m
S
Δ
Δ
y
ᄐ
ð
D
S
Þ:
With y
m
ᄐ 350 km, S
ᄐ 50 km, and R
m
ᄐ 6, 400 km, and for the first-order
triangulation, let
Δ
(D
S)
ᄐ
0.001 m; we obtain
Δ
y
ᄐ
2.34 m. In the meantime,
for the second- and third-order triangulations,
y is 23.4 m and 234 m, respectively.
Hence, the coordinates with an accuracy of 1 m and 10 m would satisfy the first-,
second-, and third-order triangulations. In a large number of computations, to avoid
accumulative errors of coordinates, the coordinates are always accurate to 0.1 m,
1 m, and 10 m. Based on the analyses above, such an accuracy of coordinates can
also satisfy the computation requirements for the arc-to-chord correction of the
same order.
Δ
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