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Precise Orbit Determination of Global Navigation Satellite System of ...

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Chapter 7 <strong>Orbit</strong> <strong>Determination</strong> Using Carrier Phase Observation<br />

order to use carrier phase observation for GEO satellite orbit determination, other independent methods such as<br />

CCD camera and SLR could be used in data preprocessing. Using these techniques, the precise distance between<br />

satellite and tracking station is obtained and the initial ambiguities <strong>of</strong> carrier phase observations can be<br />

computed. Because the tracking stations for orbit determination are located in the open area, the locked signals in<br />

the tracking stations will not be easily interrupted. Therefore initial ambiguities will not be easily changed.<br />

7.3 Ambiguity Resolution Approaches<br />

There are many ambiguity resolution approaches for GPS. Some typical methods may also be suitable for<br />

GNSS-2/Galileo orbit determination when using carrier phase measurements.<br />

Following Teunissen (1994), the ambiguity approach can be described as follows.<br />

The carrier phase measurement can be represented as<br />

ϖ ϖ<br />

Φ= r − R + c( dt− dT) + λN + ε (7-15)<br />

where<br />

ϖ<br />

r unknown receiver antenna position vector at signal reception time<br />

ϖ<br />

R given satellite antenna position vector at signal transmission time<br />

c speed <strong>of</strong> light in vacuum<br />

cdt receiver clock range <strong>of</strong>fset<br />

cdT satellite clock range <strong>of</strong>fset<br />

λ carrier wavelength <strong>of</strong> the signal<br />

N carrier phase ambiguity<br />

The term ε represents carrier phase measurement noise and biases such as satellite ephemeris errors, tropospheric<br />

and ionospheric delays, and ranging errors caused by multipath effects. In the processing <strong>of</strong> carrier phase data it<br />

is common to differentiate the carrier phase measurements between satellites and between receivers to eliminate<br />

some common errors. This gives the single and double differenced carrier phase observation equations<br />

∇Φ = ∇ r− R + c∇ dt+ λ∇ N+<br />

∇ε<br />

(7-16)<br />

∆∇Φ = ∆∇ r− R + λ∆∇N+ ∆∇ε<br />

(7-17)<br />

∇ and ∆∇ stand for the single and double difference operator. In the following discussion a two-receiver<br />

situation is assumed. The term ∇dt then denotes the single differenced clock error between the reference<br />

receiver and the remote receiver. Because <strong>of</strong> double differencing this error vanishes in Eq.(7-17). In both<br />

equations the ambiguity-terms ∇N and ∆∇N are known to be integers.<br />

Linearization <strong>of</strong> the observation equations with respect to the unknown parameters and a collection <strong>of</strong> these<br />

linearized equations into a linear system <strong>of</strong> equations gives:<br />

ϖ ϖ ϖ ϖ<br />

y = Aa+ Bb +ε (7-18)<br />

ϖ ϖ ϖ<br />

with E{} ε = 0,<br />

D{} ε = D{} y = Qy where<br />

ϖ<br />

y vector <strong>of</strong> observed minus computed differenced carrier phase observations<br />

ϖ<br />

a vector <strong>of</strong> unknown ambiguities<br />

ϖ<br />

b vector <strong>of</strong> unknown coordinates <strong>of</strong> baseline or satellite position, velocity and related<br />

dynamic parameters<br />

A,B design matrices for unknown ambiguities and parameters<br />

ϖ<br />

ε vector <strong>of</strong> unmodeled errors (in the following ϖ Qy<br />

ε is sufficiently small to be neglected)<br />

variance-covariance matrix <strong>of</strong> the observations ϖ y<br />

E{.} expectation operator<br />

D{.} dispersion operator<br />

Because ϖ a should be integers, it can be shown, that Eq. (7-18) may be solved in three steps. Firstly, estimating a<br />

double difference float solution (real-valued ambiguities ϖ ϖ<br />

a ∃ ∃b<br />

with ), i.e.<br />

ϖ ϖ ϖ 2<br />

min y− Aa−Bb with<br />

ab ,<br />

Qy<br />

ϖ ϖ<br />

ab R n<br />

, ∈ (7-19)<br />

90

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