Global Positioning System Reference
In-Depth Information
x m
b
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43
44
45
x
=
(7.94)
= N 12
12
13
b T
N 1 S
12
N 12
13
N 1 S
···
···
(7.95)
is called the double-difference float solution.
Finally, the partial derivatives of triple differences follow from those of double
di fferences by differencing
∂ϕ pq
∂ϕ pq
∂ϕ pq
km (j, i)
x m
km (j)
x m
km (i)
x m
=
(7.96)
be cause the triple difference is the difference of two double differences. The design
m atrix of the triple difference contains no columns for the initial ambiguities, because
th ese parameters cancel during the differencing.
[26
Lin
- ——
No
PgE
7. 7.3 Independent Baselines
Th e ordering scheme of base station and base satellite used for identifying the set of
independent double-difference observations is not the only scheme available. It has
been used here because of its simplicity. An example where the base station and base
satellite scheme requires a slight modification occurs when the base station does not
observe at a certain epoch due to temporary signal blockage or some other cause. If
station 1 does not observe, then the double difference
ϕ pq
23
can be computed for this
[26
pa rticular epoch. Because of the relationship
ϕ pq
23
ϕ pq
13
ϕ pq
12
=
(7.97)
th e ambiguity N pq
23
is related to the base station ambiguities as
N pq
23
N pq
13
N pq
12
=
(7.98)
In troduction of N pq
23 as an additional parameter would create a singularity of the nor-
m al matrix because of the dependency expressed in (7.98). Instead of adding this
ne w ambiguity, the base station ambiguities N pq
12 and N pq
13 are given the coefficients
1 and
1, respectively, in the design matrix. The partial derivatives with respect
to the station coordinates can be computed as required by (7.97) and entered di-
re ctly into the design matrix, because the respective columns are already there. A
si milar situation arises when the base satellite changes. The linear functions in this
ca se are:
ϕ 23
km
ϕ 13
km
ϕ 12
km
=
(7.99)
N 23
km
N 13
km
N 12
km
=
(7.100)
 
Search WWH ::




Custom Search