Global Positioning System Reference
In-Depth Information
From this n value the mean anomaly can be found from Equation (4.23) as
M
=
M 0 +
n(t c
t oe )
( 4 . 34 )
where M 0 is in the ephemeris data. In this equation t c is used instead of t as t is
not derived yet.
The eccentric anomaly E can be found from Equations (3.29) or (3.30) through
iteration as
=
+
E
M
e s sin E
( 4 . 35 )
where e s is eccentricity of the satellite orbit, which can be obtained from the
ephemeris data. Let us define a constant F as
= 2 µ
c 2
10 10
sec /( meter ) 1 / 2
F
=−
4 . 442807633
×
( 4 . 36 )
where µ is the earth's universal gravitational parameter and c is the speed of
light. The relativistic correction term is
Fe s a s sin E
t r
=
( 4 . 37 )
The overall time correction term is
t oc ) 2
t
=
a f 0 +
a f 1 (t c
t oc )
+
a f 2 (t c
+
t r
T GD
( 4 . 38 )
where T GD , t oc , a f 0 , a f 1 , a f 2 are clock correction terms and T GD is to account
for the effect of satellite group delay differential. They can be obtained in the
ephemeris data. The GPS time of transmission t corrected for transit time can be
corrected as
t
=
t c
t
( 4 . 39 )
This is the time t that will be used for the following calculations.
4.9 CALCULATION OF SATELLITE POSITION ( 5,6 )
This section uses all the information from the ephemeris data to obtain a satellite
position in the earth-centered, earth-fixed system. These calculations require the
information obtained from both Chapters 3 and 4; therefore, this section can be
considered as a summary of the two chapters.
Equation (4.19) is required to calculate the position of the satellite. In this
equation there are five known quantities: r , ν
+
ω , i ,and er . These quantities
appear on the right side of the equation and the results represent the satellite
position. Let us find these five quantities.
First let us find the value of r from Equation (4.10) as
r
=
a s ( 1
e s cos E)
( 4 . 40 )
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