Global Positioning System Reference
In-Depth Information
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Combining (8.8) and (8.10) gives the linearized form
t
+
u
+
s u
+
Qu
x
=
o
(8.11)
For the purpose of distinguishing various approaches, we call the transformation
(8.8) model 1. The seven transformation parameters (
) can be
estimated by a least-squares. The Cartesian coordinates u and x are the observations.
Equation (8.11) represents a mixed model f (
x,
y,
z, s, ε,
ψ
,
ω
o . See Section 4.4 for addi-
tional explanations of the mixed model adjustment. Each station contributes three
equations to (8.8).
A variation of (8.8), called model 2, is
a , x a )
=
t
+
u 0 +
( 1
+
s) R ( u
u 0 )
x
=
o
(8.12)
[30
where u 0 is the vector in the system (u) to a point located somewhere within the
network that is to be transformed. A likely choice for u 0 is the centroid. All other
notation is the same as in Equation (8.8). If one follows the same procedure as
described for the previous model, i.e., omitting second-order terms in scale and
rotation and their products, then (8.12) becomes
Lin
1.3
——
Lon
*PgE
t
+
u
+
s ( u
u 0 )
+
Q ( u
u 0 )
x
=
o
(8.13)
Model 3 uses the same rotation point u 0 as model 2, but the rotations are about
the axes (n, e, u) of the local geodetic coordinate system at u 0 . The n axis is tangent
to the geodetic meridian, but the positive direction is toward the south; the e axis is
perpendicular to the meridian plane and is positive eastward. The u axis is along the
ellipsoidal normal with its positive direction upward, forming a right-handed system
with n and e . Similar to Equation (8.12), one obtains
[30
t
+
u 0 +
( 1
+
s) M ( u
u 0 )
x
=
o
(8.14)
If (
λ 0 ,h 0 ) are the
geodetic coordinates for the point of rotation u 0 , it can be verified that the M matrix is
η
,
ξ
,
α
) denote positive rotations about the (n, e, u) axes and if 0 ,
R 3 (
λ 0 ) R 2 ( 90
M
=
ϕ 0 ) R 3 (
α
) R 2 (
ξ
) R 1 (
η
) R 2 ( 90
ϕ 0 ) R 3 (
λ 0 )
(8.15)
Since the rotation angles (
η
,
ξ
,
α
) are differentially small, the matrix M simplifies to
M (
λ 0 0 ,
η
,
ξ
,
α
)
= α
M α + ξ
M ξ + η
M η +
I
(8.16)
where
λ 0
0
sin ϕ 0
cos ϕ 0 sin
M α =
sin ϕ 0
0
cos ϕ 0 cos
λ 0
(8.17)
cos ϕ 0 sin
λ 0
cos ϕ 0 cos
λ 0
0
 
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