Geoscience Reference
In-Depth Information
"
#
2
3
2
dy
dx
1
þ
x 0
R x 0
:
d 2 y
dx 2
x 0
Derivations of the Formula
Transformation Between Coordinate Systems P-xyz and O-XYZ
The equation of the ellipsoid in the coordinate system P-xyz cannot be computed
unless the relationship of transformation between the coordinate systems O-XYZ
and P-xyz is determined. As shown in Fig. 5.10 , let P be a point on the initial
meridian (the coordinate plane XOZ); PK is the normal passing through P, PK
N,
e 2 ), and the coordinate values of point P can be obtained from
PQ
N(1
Fig. 5.10 :
2
3
2
3
X
Y
Z
N cos B
0
4
5
4
5 :
e 2
N 1
ð
Þ
sin B
As shown in Fig. 5.10 , in order to make point P coincide with point O, the origin
of the coordinate system P should be translated to the point O. To make the
coordinate plane xPz coincide with the meridian, the coordinate system should be
rotated with a negative angle A around the z-axis. Similarly, for the z-axis, which is
directed towards the normal, parallel to the minor axis of the ellipsoid, the coordi-
nate system should be rotated by an angle of 90 + B about the y-axis. P-xyz is
thereby transformed into O-XYZ, given by:
2
3
2
3
2
3
X
Y
Z
x
y
z
N cos B
0
R z
4
5
R y 90
4
5 þ
4
5
þ
B
ðÞ
A
e 2
N 1
ð
Þ
sin B
2
3
2
3
sin B cos A
sin B sin A
cos B
x
y
y
4
5
4
5
sin A
cos A
0
cos B cos A
cos B sin A
sin B
2
3
N cos B
0
4
5 :
þ
ð
5
:
24
Þ
e 2
N 1
ð
Þ
sin B
Namely:
Search WWH ::




Custom Search