6.4.6 Dual Frequency Relations

OTHER DUAL FREQUENCY PHASE COMBINATIONS



There are other linear combinations of L1 and L2 observables that could be constructed, leading to a variety of observables with different wavelengths, ionospheric amplification factors and data noise characteristics (see, for example, ABIDIN, 1993). Desirable features of the artificial observables that can be constructed from the L1 and L2 observations, for data processing purposes, are:


The linear combinations of the L1 and L2 phases which preserve the integer nature of the cycle ambiguity, can be expressed as (in units of cycles):

i,jm = i.(L1) + j.(L2) (6.4-22a)

where i and j are integer constants. The following are some properties of the linear combination observables (ABIDIN, 1993).


The cycle ambiguity:

ni,j = i.n1 + j.n2 (6.4-22b)


The frequency:

fi,j = i.f1 + j.f2 (6.4-22c)


The effective wavelength:

i,j = c / fi,j (6.4-22d)


The ionospheric effect:

(6.4-22e)


The ionospheric scale factor isf:

dion(i,j) = isf.dion(L1)

where

(6.4-22f)


The noise scale factor nsf:

(i,j) = nsf.(1)

where

(6.4-22g)

and (1) is the standard deviation of the L1 phase observation ( in metres, and assuming equal noise on L1 and L2 when expressed in metric units).


The parameters in the columns in Table below have been computed using the relations in eqn (6.4-22).


Some common linear combinations of L1 and L2 phase observations.
Phase
Combination
i,j
(m)
Noise
nsf x L1
Ion. delay
isf x dion(L1)
Ambiguity
L1 0.190 1.0 1.0 n1
L2 0.244 1.28 1.65 n2
L3 0.190
0.244
3.2 0.0
(or)
1n1 + 2n2
1n1 + 2n2
L4 1.63 -0.65 1n1 + 2n2
L5 0.862 6.4 -1.28 n1 - n2
L6 0.107 0.8 1.28 n1 + n2

nsf is the noise scale factor to relate the data "noise" of the linear combination to that of the L1 observation
isf is the magnitude of the ionospheric scale factor needed to relate the ionospheric delay on the linear combination to the ionospheric delay on the L1 observation.


Some well known linear combinations are:

> wide-lane: i = 1, j = -1 (L5)
> narrow-lane: i = 1, j = 1 (L6)
> first GPS signal: i = 1, j = 0 (L1)
> second GPS signal: i = 0, j = 1 (L2)
> double wide-lane: i = -3, j = 4
> half wide-lane: i = 2, j = -2
> semi wide-lane: i = -1, j = 2
> ionosphere-free: i =77, j =-60
> "monster" wide-lane: i = -7, j = 9

 

Two interesting combinations are worth closer inspection. The "monster wide-lane" combination has the largest of all the wavelengths, being of the order of 14.65m! However, it suffers in two respects: (a) the noise scale factor is about 350 (if the noise on L1 is 1mm, the noise on -7,9 is 0.35m!), and (b) the ionospheric bias is approximately 870 times the delay on L1! An analysis eqn (6.4-22e) results in another ionosphere-free combination that can be constructed with integer coefficients i = 77, j = -60. The effective wavelength of the 77,-60 combination is very small, 77,-60 0.006m.

A number of linear combinations of L1 and L2 observations derived from certain codeless GPS receivers, for which the effective wavelength of the L2 measurement is half that of the L2 signal, are useful. For example, the "half wide-lane" is the linear combination that is analogous to the standard L5 combination, constructed using the full wavelength L1 and the half wavelength L2 measurement. The effective wavelength of this combination is 43cm, however the ionospheric scale factor and the noise scale factor are the same as for the L5 combination.

The more "exotic" dual-frequency combinations will not be discussed in these notes. Some useful combinations of dual-frequency phase and dual-frequency pseudo-range data will be introduced in the next section.

 

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© Chris Rizos, SNAP-UNSW, 1999