Global Positioning System Reference
In-Depth Information
The true anomaly can be found from Equation (4.41) as
ν 1 = cos 1 cos E
e s
1
e s cos E
sin 1 1 e s sin E
1
ν 2 =
e s cos E
ν
=
ν 1 sign 2 )
(9.14)
and angle φ can be found from Equation (4.42) as
π
ν
+
ω
( 9 . 15 )
where ω is the argument of perigee (subframe 3, bits 197 - 204 and 211 - 234)
obtained from navigation data.
The following correction terms are needed as shown in Equation (4.43):
=
+
δφ
C us sin 2 φ
C uc cos 2 φ
δr
=
C rs sin 2 φ
+
C rc cos 2 φ
δi
=
C is sin 2 φ
+
C ic cos 2 φ
(9.16)
where C us (subframe 2, bits 211 - 226), C ue (subframe 2, bits 151 - 166), C rs
(subframe 2, bits 69 - 84), C rc (subframe 3, bits 181 - 196), C is (subframe 3,
bits 121 - 126), and C ic (subframe 3, bits 61 - 76) are obtained from navigation
data. These three terms are used to correct the following terms as shown in
Equations (4.44) and (4.45):
φ φ + δφ
r
r
+
δr
i
i
+
δi
+ idot (t
t oe )
(9.17)
where idot (subframe 3, bits 279 - 292) is the rate of inclination angle and is
obtained from the navigation data, t is obtained from Equation (9.13).
The angle between the accenting node and the Greenwich meridian er can
be found from Equation (4.46) as
˙ (t
˙ ie t
er
=
e
+
t oe )
( 9 . 18 )
The final two steps are to find the position of the satellite from Equation (4.47)
and adjust the pseudorange by the overall clock correction term as
x
y
z
r cos er cos φ
r sin er cos i sin φ
=
r sin er cos φ
+
r cos er cos i sin φ
r sin i sin φ
ρ i
ρ i
+
ct
(9.19)
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