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The GNSS integer ambiguities: estimation and validation

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with ep a p-vector with ones, Ip an identity matrix of order p, <strong>and</strong>:<br />

⎛<br />

µ = T ⎜<br />

µ1 · · · µf , Λ = ⎝<br />

λ1<br />

. ..<br />

λf<br />

⎞<br />

⎟<br />

⎠ (2.36)<br />

In the same way the geometry-based model is obtained, but the observations collected in<br />

the vector y are now the observed-minus-computed observations from equation (2.22).<br />

<strong>The</strong> model is given by:<br />

<br />

µ<br />

E{y} = (e2f ⊗ G) ∆rqr + (e2f ⊗ Im) T + ⊗ Im I<br />

−µ<br />

<br />

(2.37)<br />

0<br />

+ (I2f ⊗ em) dtqr + ⊗ Im a<br />

Λ<br />

with<br />

G = −u 1 qr · · · −u m qr<br />

T<br />

<strong>and</strong><br />

−(u s r) T ∆rr + (u s r) T ∆r s − −(u s q) T ∆rq + (u s q) T ∆r s<br />

= −(u s qr) T ∆rqr − (u s qr) T ∆rq + (u s qr) T ∆r s<br />

≈ −(u s qr) T ∆rqr,<br />

(2.38)<br />

(2.39)<br />

since the orbital uncertainty ∆r s can be ignored if the baseline length rqr is small<br />

compared to the satellite altitude (Teunissen <strong>and</strong> Kleusberg 1998). <strong>The</strong> term with the<br />

receiver position error ∆rq is zero when the position of receiver q is assumed known. <strong>The</strong><br />

parameters in ∆rqr are referred to as the baseline increments; if the receiver position rq<br />

is known, the unknown receiver position rq can be determined from the estimated ∆rqr.<br />

Both single difference models (2.35) <strong>and</strong> (2.37) are rank deficient. <strong>The</strong> rank deficiencies<br />

can be resolved by lumping some of the parameters <strong>and</strong> then estimate these lumped<br />

parameters instead of the original ones. <strong>The</strong> parameters are lumped by performing<br />

a parameter transformation, which corresponds to the so-called S-basis technique as<br />

developed by Baarda (1973) <strong>and</strong> Teunissen (1984).<br />

A first rank deficiency is caused by the inclusion of the tropospheric parameters. This<br />

can be solved for the geometry-free model by lumping the tropospheric parameters with<br />

the ranges:<br />

ρ = ρ1 qr + T 1 qr · · · ρm qr + T m T qr<br />

(2.40)<br />

In the geometry-based case, the tropospheric delay parameter is first reparameterized<br />

in a dry <strong>and</strong> wet component. <strong>The</strong> dry component is responsible for about 90% of the<br />

tropospheric delay <strong>and</strong> can be reasonably well corrected for by using a priori tropospheric<br />

models, e.g. (Saastamoinen 1973). <strong>The</strong> much smaller wet component is quite variable<br />

16 <strong>GNSS</strong> observation model <strong>and</strong> quality control

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