08.06.2013 Views

Bernese GPS Software Version 5.0 - Bernese GNSS Software

Bernese GPS Software Version 5.0 - Bernese GNSS Software

Bernese GPS Software Version 5.0 - Bernese GNSS Software

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

2.3.6.3 Wide-Lane Linear Combination L5<br />

The linear combination<br />

L5 =<br />

1<br />

f1 − f2<br />

2.3 Observation Equations<br />

(f1 L1 − f2 L2) (2.47)<br />

is used in the <strong>Bernese</strong> <strong>GPS</strong> <strong>Software</strong> on the double-difference level for phase observations<br />

to fix cycle slips and to resolve ambiguities to their integer values. Using Eqns. (2.37c) and<br />

(2.37d) and neglecting both, the ionospheric refraction I ij<br />

kℓ and the tropospheric refraction<br />

∆̺ ij<br />

kℓ , we obtain<br />

L ij<br />

5kℓ = ̺ij<br />

kℓ +<br />

c<br />

(n<br />

f1 − f2<br />

<br />

λ5<br />

ij<br />

1kℓ − nij<br />

2kℓ )<br />

<br />

n ij<br />

. (2.48)<br />

5kℓ<br />

The formal wavelength λ5 is about 86 cm and is roughly four times larger than λ1 or λ2.<br />

Therefore, this linear combination is called wide-lane combination and the corresponding<br />

ambiguity<br />

is called wide-lane ambiguity.<br />

n ij<br />

5kℓ = nij<br />

1kℓ − nij<br />

2kℓ<br />

2.3.6.4 Melbourne-Wübbena Linear Combination L6<br />

(2.49)<br />

The Melbourne-Wübbena combination is a linear combination of both, carrier phase (L1<br />

and L2) and code (P1 and P2) observables as described by [Wübbena, 1985] and [Melbourne,<br />

1985]. This combination eliminates the effect of the ionosphere, the geometry, the clocks,<br />

and the troposphere. The combination is given by<br />

L6 =<br />

1<br />

f1 − f2<br />

(f1 L1 − f2 L2) −<br />

For double-difference observations, we obtain<br />

1<br />

f1 + f2<br />

(f1 P1 + f2 P2) . (2.50)<br />

L ij<br />

6kℓ = λ5 n ij<br />

5kℓ . (2.51)<br />

With “good” P-code data (rms ≤ 1 m) this linear combination may be used for the resolution<br />

of the wide-lane ambiguities n ij<br />

5kℓ . On the zero-difference level, the same linear combination<br />

gives<br />

(2.52)<br />

L i 6k = λ5 n i 5k<br />

which means that this linear combination may be used to check zero-difference observations<br />

for cycle slips. However, only the difference ni 1k − ni 2k can be checked in this way.<br />

The most important linear combinations and their characteristics are summarized in Table<br />

2.10. The specifications with respect to “noise” and “ionosphere” are based on units of<br />

meters. L1 and L2 (expressed in meters) are assumed to be equally accurate and uncorrelated.<br />

Note that the noise of “L6” is given relative to that of P1 and P2, respectively, since<br />

this noise level is pre-determined exclusively by the quality of the P-code data considered<br />

(compare also Eqn. (2.50)).<br />

<strong>Bernese</strong> <strong>GPS</strong> <strong>Software</strong> <strong>Version</strong> <strong>5.0</strong> Page 41

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!