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
(ν
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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