Journal of Global Positioning Systems (2003)
Vol. 2, No. 2: 100-108
Datum Definition in the Long Range Instantaneous RTK GPS
Network Solution
Israel Kashani1,2, Pawel Wielgosz1,3, Dorota Grejner-Brzezinska1
1 The Ohio State University, CEEGS, 470 Hitchcock Hall, 2070 Neil Avenue, Columbus, OH 43210-1275
e-mail: kashani.1@osu.edu, tel.: 614-292-0169, fax: 614-292-2957
2 Technion - Israel Institute of Technology
3 University of Warmia and Mazury in Olsztyn, Poland
Received: 17 October 2003 / 16 December 2003
Abstract. This paper presents the multiple reference
station approach to wide area (and regional)
instantaneous RTK GPS, implemented in the MPGPSTM
(Multi Purpose GPS Processing Software) software,
developed at the Ohio State University. A weighted free-
net approach (WFN) was applied in the instantaneous
RTK software module, which enabled optimal estimation
of the rover coordinates, properly reflecting the
accuracies of the observations and the coordinates of the
CORS stations. The effect of using the distance-
dependent weighting scheme in the WFN approach on
the final rover solution is analyzed. The influence of the
different weights was studied by introducing the
distance-dependent weights as a function of the CORS
station separation L to the rover (1/L2). The results show
that almost 100% of the differences between the
computed horizontal rover coordinates and the known
reference coordinates are below a decimeter, and 95% of
the differences in the vertical coordinate are below 20
cm, when using the suggested approach. In addition, the
accuracy analysis of two other solutions, with different
datum definition (minimum constraint and over-
constrained), is presented. This analysis verifies the
suitability of the stochastic models used in the RTK
module and the rigorous approach, taking into account
inter-baseline correlation as well as the correlation in-
between each baseline component.
1 Introduction
1.1 RTK GPS Positioning
The most challenging mode among all the kinematic GPS
techniques is long range instantaneous RTK, while no
data accumulation is made throughout the adjustment
process. With longer distances to the reference stations,
the RTK technology faces great challenges, since many
distance-dependent biases (atmospheric, orbital errors,
etc.) need to be precisely modeled. If not properly
accommodated, these effects may seriously corrupt the
positioning and time transfer results. The success of
precise GPS positioning over long baselines depends on
the ability to resolve the integer phase ambiguities when
short observation time spans are required, which is
especially relevant to RTK applications (IAG SSG 1.179,
2000-2003). Instantaneous ambiguity resolution has
several advantages over the on-the-fly (OTF) method; it
is resistant to negative effects of cycle slips and can
provide immediate centimeter level positioning accuracy
without any delay needed for initialization as required by
the OTF technique (Pratt et al., 1998). However, the
ambiguity resolution can only be achieved if the
atmospheric, orbital and timing errors are properly
accounted for.
Over the past few years, the use of a GPS reference
station network approach has shown great promise in
extending the inter-receiver separation. The
implementation of multiple reference stations in a
permanent array offers several advantages over the
standard single-baseline approach. It improves the
accuracy of the mobile receiver and makes the results less
sensitive to the length of the rover-reference baselines
(Chen et al., 2000; Dai et al., 2001; Cannon et al., 2001).
Consequently, the precision of the baseline components,
Key words: RTK, GPS, Datum Definition
Some results presented here were reported at ION GNSS 2003, Portland, OR
Kashani et al.: Datum Definition in the Long Range Instantaneous RTK GPS Network Solution 101
in terms of their standard deviation is improved. The
most important contribution of the network solution, as
compared to the baseline approach, is not, however, the
improvement in precision, but rather the improvement in
the reliability and availability, as well as the new
possibilities for modeling atmospheric errors (Marel,
1998). Moreover, it is still possible to get an acceptable
solution even if there are gaps, outliers or cycle slips in
some of the reference station data.
1.2 Geodetic Control and Datum Definition
Observation equations relating to any geodetic network
are normally rank-deficient due to the lack of datum
reference. There is, therefore, a need to define the datum
in order to solve for the positioning parameters. Datum
definition can be accomplished by a careful selection of
some constraints added to the observation equation
model. This could be done while fixing one or more
reference stations during the adjustment procedure. When
only one reference station is held fixed we establish a
datum referred to as a minimum constraint solution; if
more than one station is fixed, the datum will be referred
to as an over-constrained solution. For a free network
approach, it is often desirable that the property of the
minimum sum of the variances and minimum sum of
squares of the correction to the coordinates is restricted to
certain points (Koch, 1999). These points are
undoubtedly those that correspond to the reference points
in the geodetic network. When dealing with GPS
multiple reference station processing, the CORS stations
should be considered a high order reference network.
Free net adjustment techniques play a major role in the
analysis of geodetic networks. Free networks are very
popular in geodesy, surveying and mapping, mainly due
to their unique property of being independent of errors in
external data. The results of the free net adjustment and
their superior quality serve as an authentic reflection
(undistorted mirror image) of the measurement quality
(Papo, 1999). There are several unique properties of the
free networks, as follows:
The estimated accuracies of the coordinates are
optimal (Meissl, 1969). They depend solely on the
actual accuracies of the measurements. One of the
most important properties of a free network adjustment
is that of generating the minimum trace in the
dispersion matrix of the unknowns (Fritsch and
Schafrin, 1982).
They are an unbiased representation of the adjusted
measurements.
The coordinates of the network points define the
coordinate system. A more flexible approach may be
adopted by applying weights to these coordinates
(WFN).
In order to evaluate the quality and effectiveness of the
WFN approach, two more methods using different, datum
definition were tested; these are the minimum constraints
(MC) and the over-constrained (OC) methods, and the
comparison between the three models was carried out.
The results show noticeable improvements with respect
to the mean and standard deviation (STD) in the
estimated rover coordinates while using the suggested
WFN approach.
1.3 The MPGPSTM Software
The MPGPSTM software, currently under development at
OSU, includes different processing modules. The primary
goal of the development of the instantaneous RTK
module is to achieve reliable instantaneous real-time
solutions for distances over 100 km from the reference
stations. In order to accomplish this goal, a multi-
reference station approach is implemented. This paper
presents the test results from the current software
implementation, based on the actual field data. The
results analyzed here were obtained using instantaneous
processing and the ambiguity resolution technique in the
post-processing mode. The method is, however, suitable
for real time.
At the current stage of the software development, we
assume a unidirectional radio link from the reference
network stations (CORS) to the user receiver (rover). The
implemented algorithm is based on the double-
differences (DD) mode, which requires receiving
observations from one or more reference stations (i.e.
baseline or network solution). It should be noted that all
the processing is carried out at the rover. The
applicability of the unidirectional radio link was tested by
the Federal Highway Administration (FHWA) over long
distance, and real-time kinematic application was
demonstrated at 250 km (Remondi, 2002).
The ongoing developments of the MPGPSTM software
include transmitting the DD atmospheric corrections
derived from the reference network stations. These
corrections may further increase the system capabilities,
allowing for increased rover-network distances.
1.4 The VCV Matrix
The reliability of the variance-covariance (VCV) matrix
of the estimated parameters is of great importance,
especially in a multi-station processing mode (i.e.
network-based solution), when several baselines are
processed together (Kashani, 2002). The estimation of a
realistic VCV matrix by GPS processing software is a
function of the measurement weights (e.g. phase and
code) and the stochastic models taking into account both
mathematical and physical correlation between the
102 Journal of Global Positioning Systems
measurements. While the mathematical correlation can be
easily modeled, the physical correlation, unfortunately, is
more complicated to model. Consequently, if simplified
stochastic models are used, overly optimistic statistics
might result even in more comprehensive software,
which processes the measurements in a multi-station
mode, and produce a fully populated VCV (i.e.
considering the between baselines mathematical
correlation).
VCV matrices derived from a number of the existing
GPS software might not be realistic, especially in the
case of commercial packages (Howind et al., 1999). The
practical implication is that the produced accuracies are
too good, while the derived coordinates are in fact less
accurate. Therefore, a wrong decision could be made,
based on the software-derived accuracies, that the
solution the software presents is reliable and acceptable.
The majority of the GPS processing software packages
consider the VCV matrix of the observations to be either
diagonal - i.e., no correlation is considered, or block
diagonal - i.e., only the mathematical correlation is
considered (El-Rabbany et al., 2003).
All the modules in the MPGPSTM software include
rigorous stochastic models. The stochastic model used in
the network-based RTK module, which is based on DD
measurements, includes the inter-baseline mathematical
correlation (i.e., fully populated matrix). Even though,
the physical correlations are not taken into account, the
presented accuracy analysis indicates that the VCV
matrix seems realistic, rendering convincing coordinate
standard deviations.
2 Methodology
In this section, the review of the parameter estimation
procedure based on the model of DD GPS observations is
given, with a particular emphasis on different network
adjustment strategies. In general, the instantaneous RTK
software Module consists of three major steps as
presented by Kashani et al. (2003):
1. Float solution - based on network adjustment.
2. Integer ambiguity estimation - using the classical
wide-lane and 60/77 search algorithm.
3. Fixed solution - network adjustment introducing the
fixed ambiguities.
The parameter estimation is carried out by the least-
squares principle. An elevation-depended stochastic
model (weighting scheme) and mathematical correlation
including inter-baseline and baseline-component
correlations were taken into account and applied in the
algorithm. In addition, a fast Cholesky decomposition
was applied during the adjustment process. The network
solution was performed including all the independent
baselines in the network (i.e. from all the reference
stations to the rover).
2.1 Instantaneous RTK
2.1.1 Float Network Solution
The instantaneous RTK algorithm requires the use of
both the pseudo-range and phase observations due to the
low redundancy. Hence, the DD observation equations
for the GPS measurements are as follows:
1,1 1,
22
2,122 2,
1,
22
2,1 2
(/)
(/)
klklkl klkl
ijij ijijij
klkl klklkl
ijij ijijij
klklkl kl
ijij ijij
klkl klkl
ijij ijij
TI N
TffI N
PTI
PTffI
Φρ λ
Φρ λ
ρ
ρ
=+− +
=+− +
=++
=++
(1)
Where:
,
kl
nij
Φ
DD phase observation on frequency n (n=1,2)
,
kl
nij
P DD code observation on frequency n
kl
ij
ρ
DD geometric distance
kl
ij
T DD tropospheric delay
kl
ij
I
DD ionospheric delay
12
,ff
first and second GPS frequencies
while i,j denote the two receivers and k,l the two
satellites.
The Modified Hopfield model was used to calculate the
tropospheric DD corrections (T), and the DD
ionospheric delay (
kl
ij
kl
ij
I
) parameters were estimated in the
adjustment procedure. Thus, the adjustment model
becomes a simple one including only three types of
unknowns: rover coordinates (and some reference station
coordinates in the MC and the WFN), DD ambiguities,
and the DD ionospheric delay parameters.
The system of observation equations, which after
linearization with respect to the unknown parameters
gives the linear system of equations, is presented in
equation (2):
VLAX
+
= (2)
Where:
L Measured minus computed measurement
V Measurement corrections
Kashani et al.: Datum Definition in the Long Range Instantaneous RTK GPS Network Solution 103
A Design matrix relating measurements and
coordinates 11,2,
21,
ˆˆ
()
ˆˆ
(6077 )
kl kl
ij ij
kl kl
ij ij
Kround NN
K round NN
=−
=−
2,
X Corrections to the approximate unknowns
This approach deals with the DD code and phase
measurements from one pair of satellites and receivers at
a time that we call “one at a time” approach. Thus, at this
stage the network was decomposed to individual DD
pairs in order to fix the ambiguities. Although only a
particular combination yields the correct integer solution
for the two ambiguity sets, the 1
and 2
K
values may
not be free of errors. Consequently, not all of the
ambiguities can be recovered to their correct integer
values, especially for longer baselines. However, in the
test data analyzed here, almost all the ambiguities (96%)
were successfully fixed to their integer values. Since the
primary objective of this paper is the demonstration and
performance of the WFN approach, we do not
concentrate on the ambiguity search and validation
techniques here, but rather on the practically achievable
accuracy within the current software/algorithmic
configuration.
The unknown parameters X and the corresponding design
matrix A could be subdivided with respect to the
unknown ambiguities and the remaining parameters (i.e.,
the baseline components and the ionospheric delay
parameters), as follows:
112 2
VLAx Ax+= + (3)
Where 1
x
and the corresponding design matrix 1
A
refer
to the ambiguities; 2
x
and the corresponding design
matrix 2
refer to the remaining parameters.
As a result of the float network solution, real valued
estimates for both the ambiguities and the baseline
components are obtained, together with their
corresponding VCV matrices. Following Teunissen
(1998), the resulting float network adjustment solution
and its VCV matrix will be:
112
21 2
ˆˆˆ
1
ˆˆ ˆ
2
ˆ;
ˆ
xxx
xx x
QQ
x
xQQ

 
 
 
(4)
2.1.3 Fixed Solution
Once the fixed solution 1
x
has been obtained, as
described in the previous section, the ambiguity residuals
(1
ˆ
x
-1
x
) are used to correct the float solution 2
x
in order
tofinal positioning solution for the rover, prod
22
ˆ
uce the
1
()
x
xx
=

, shown in equation (6) (Teunissen 1998):
The solution of the integer least-squares problem is
denoted as 1
x
and 2
x
; the corresponding float solution is
denoted as 1
ˆ
x
and2
ˆ
x
; 1
ˆ
x
Q is the VCV matrix of1
ˆ
x
; 2
ˆ
x
Q
is the VCV matrix of2.
ˆ
x
12 1
1
ˆˆˆ
221 211
ˆˆ ˆ
()( )
xx x
x
xxxQQxx
==− −
 
(6)
2.1.2 Wide-Lane Ambiguity Search This equation refers to the relationship between the float
and the fixed solutions. It shows how the deference
between these two rover coordinate estimates depends on
the difference between the real-valued least squares
ambiguity estimates, 1
ˆ
x
, and the integer least-squares
ambiguity estimate,1
x
. In order to get the VCV matrix of
2
x
1
ˆ
one should apply the law of error propagation to (6) as
follows:
At this stage of the algorithm, the real-valued ambiguities
1
ˆ
x
, denoted as and , from the float network
solution are fixed to their integer values,
1,
ˆkl
ij
N2,
ˆkl
ij
N
1
x
, designated
as and . This step follows the classical wide-
lane and 60/77 search method with the integer
approximation on baseline-by-baseline basis (Yang et al.,
1994):
1,
kl
ij
N
2,
kl
ij
N
221212
1
ˆˆˆˆˆ
x
xxxxx
QQQQQ
=−
x
(7)
2,1 2
1,2, 1
(60) /17
kl
ij
kl kl
ij ij
NKK
NNK
=−
=+ (5)
2.2 Free-Net Adjustment Approach
Where:
The mathematical model of n measurements, which
produces a set of n observation equations linearized at the
approximated values of the coordinates, is given in
equation (2). The basis of the null space of A (Papo,
1,
kl
ij
N and are the integer ambiguities from the center
of the search space.
2,
kl
ij
N
104 Journal of Global Positioning Systems
According to Wolf (1977), any two X vectors, which
pertain to two different datums - for example, Xm and Xk,
- are related through the following simple equation:
1987), known also as the Helmert transformation matrix
E, has the following important property:
0AE = (8)
Datum based on selected m points is defined by
subjecting the vector X in (2) to the following linear
constraints (Papo and Perelmuter, 1981; Papo, 1986;
Papo, 1989):
0
TT
mm
EPXE X== (9)
where:
mm
EP=E
m
and
T
mm
PP=
mk k
X
XEt
=
+ (12)
where tkm is a d vector containing transformation
parameters from the k - to the m - datum. The solution for
tkm is derived from (12) under the minimum condition
(10), as follows (Wolf, 1977 and Papo, 1987):
1
()
TT
kmmmkm k
tEEEXH
=−=− X (13)
When using a network-based approach with CORS
stations in RTK mode, only the CORS station coordinates
should be used to establish a datum, and the solution
should be the m-datum one, as presented in equation (9).
The Pm diagonal matrix entries include zeros or ones, and
define the datum points by setting ones in the correct
places. This solution is known as a “Weighted Free Net”
(WFN) adjustment. However, the Pm matrix could be
populated by different weights for the datum-defining
points, such as distance-dependent weights, as presented
here. Moreover, any a priori information, such as VCV
matrix of the CORS station coordinates, could also
replace the respective entries in the Pm matrix (Kashani,
2002).
Equation (10) is derived from seeking a minimum of the
following quadratic form:
min.
T
m
XPX= (10)
First, we minimize the VP quadratic form in order to
create the set of normal equations:
TV
NX U= (11)
The above set is singular due to the need for datum
definition. It can be solved only if we apply at least d
independent linear constraints, as the order of the datum
defect to X. If, for example, we apply (9) to (11), we will
obtain a particular solution denoted as Xm. There is an
infinite number of sets of d constraints, which, when
applied to (11), will produce different solution vectors X,
all of which satisfy the normal equation (11).
3 Experiment
3.1 Data Source
The results shown herein were generated from
a static network of the Ohio CORS
(http://www.dot.state.oh.us/aerial/Cors.asp). In addition
to the three reference stations: SIDN, COLB and LEBA
from the Ohio CORS, a City of Dayton CORS static
station served as a rover. Figure 1 shows the test network
with the analyzed baselines marked. All the stations were
equipped with TRIMBLE 5700 high quality geodetic
receivers and antennas. The reference stations were
equipped with choke-ring GPS antennas, and the Dayton
station was connected to a geodetic antenna.
Let us consider one particular branch of such solutions,
which is characterized by the contents of the Pm weight
matrix. Out of the multitude of Pm matrices (and
respective datums), there is one particular solution, which
is unique, since the Pm matrix is equal to the identity
matrix. We will denote that unique solution as Xk. In this
case, m=k when each of the k points in the network
contributes to the datum definition on an equal basis, as
Pk=I.
Meissl (1969) and Koch (1999) have shown that such a
solution, as compared to the rest of the existing solutions,
is optimal and unique in the sense that the trace of the
VCV matrix is minimum. In addition, it can be shown
(Koch, 1999) that Qk, the un-scaled (σ0
2) VCV matrix of
X, is the pseudo-inverse of N, known also as the Moore-
Penrose inverse of N (Qk = N+). According to Meissl
(1969), the above optimal solution is the only one that
faithfully reflects the accuracy of the measurements,
where all the other (external) sources of error have been
effectively filtered out.
This reference-rover configuration reflects a possible
scenario common in surveying practice. Precise dual
frequency data collected on August 03, 2003 at a
sampling rate of 30-seconds for 13 hours between 00:00-
13:00 UT were used. A total of 1588 observation epochs
with the phase-smoothed code (Springer, 1999) and
carrier phase measurements were processed and
analyzed. The distances between the reference stations
varied from 98 to 121 km, and the distances to the rover
ranged from 40 to 100 km. The GPS data were collected
under moderate geomagnetic and ionospheric conditions
with the maximum Kp value reaching 3+.
Kashani et al.: Datum Definition in the Long Range Instantaneous RTK GPS Network Solution 105
Fig. 1 Test area map.
4 Analysis of the Results
In order to analyze the performance of the WFN
approach, two other models, MC and OC, were
introduced and tested against the WFN model. The
influence of a weighting scheme was studied by
introducing distance-dependent weights as a function of
the CORS station separation L from the rover (1/L2). The
final rover solution is analyzed in terms of the deviation
of the estimated coordinates from the reference truth, and
the reliability of their estimated uncertainties. Three
models were tested as follows:
60km
40km
100km
a) MC - only the closest to the rover CORS station was
fixed.
b) OC - all the CORS stations were fixed.
c) WFN - distance-dependent weighting scheme, where
the reference stations serve as datum-defining points.
The mean and the standard deviations based on the
processed time series of the rover coordinate components
(n,e,u) were calculated to compare the different models.
The results obtained for the three cases (a, b and c) are
shown in Tables 1 and 2; graphical presentation is shown
in Figure 2. In addition, Figure 3 presents a scatter plot of
the n,e components derived using the WFN approach.
What is immediately noticeable in Figure 2 is that the
WFN produces the most stable and the least noisy
05001000 1500
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
dn, de [m]
Minimum
Constraints
05001000 1500
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
Over
Const rained
05001000 1500
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
Weighted
F ree-Net
05001000 1500
-0.4
-0.2
0
0.2
0.4
du [m]
05001000 1500
-0.4
-0.2
0
0.2
0.4
05001000 1500
-0.4
-0.2
0
0.2
0.4
du
du
du
dn
de
dn
de
dn
de
EpochsEpochs
Fig. 2 Comparison of n,e (left side) and u (right side) components derived using different constraints in epoch by epoch mode.
106 Journal of Global Positioning Systems
solution both in the horizontal and vertical components,
as compared to the other two models. The absolute means
of the calculated rover position residuals (the differences
from the known position) equal to 3.1 cm and 2.3 cm for
east and north components, respectively. This is about
15-20 percent improvement as compared to the OC
method (the second best) and about 30-40 percent better
than the MC. The STD time series is also the lowest for
the WFN in all three components. As one could expect,
the height component is the less accurate (~ 2-3 times)
than the horizontal one.
Table 2. Standard deviations of n,e,u components derived using
methods with different constraint schemes.
Time series STD [m]
ComponentMC OC WFN
n 0.065 0.050 0.045
e 0.041 0.033 0.030
u 0.174 0.143 0.131
Table 3. Summary statistics of the coordinate residuals; threshold level
of 10 cm and 20 cm was applied to the horizontal and the height
components, respectively.
-0.5 -0.4 -0.3 -0.2 -0.100.1 0.20.30.4
-0.2
-0.15
-0.1
-0.05
0
0.05
0.1
0.15
WFN - n,e scatter plot
[m]
[m]
Percentage
ComponentMC OC WFN
n (10 cm) 88 96 98
e (10 cm) 96 99 100
u (20 cm) 85 91 95
The obtained accuracy analyses are presented in Figure 4,
which shows the derived n,e,u residuals, obtained using
all three models, versus ±3σ limit. The plots in Figure 4
show high correlation between the residuals and the
estimated STDs, and also confirm that the WFN approach
provided optimal accuracies, as compared to the MC and
the OC methods. The results prove that the rigorous
stochastic model used in the instantaneous RTK module
is correct.
Fig. 3 Scatter plot of the n,e components derived using the WFN
approach in epoch by epoch mode.
5 Summary and Conclusions
In order to investigate the capabilities of the
instantaneous RTK algorithm presented here, a success
rate analysis was performed. Table 3 presents summary
statistics of the residual time series, represented as the
success rate of the true coordinate recovery by the
different models. The horizontal threshold was set to 10
cm and the vertical one to 20 cm. The results presented in
Table 3 confirm that the WFN approach performs the
best with about 98-100 percent success rate in the
horizontal components and 95 percent in the vertical one.
The results presented here were based on the analyses of
13 hours of dual-frequency GPS data collected at the
Ohio CORS and the Dayton CORS stations. The data
were processed with the beta version of the MPGPSTM
software; the multi-base instantaneous RTK module was
used. It should be noted that no data accumulation was
applied during the processing, thus a one-epoch solution
was carried out for all 1588 observed epochs (i.e., every
epoch is considered independent from the previous epoch
solution). The distances between the reference stations
varied from 98 to 121 km, and distances to the rover
ranged from 40 to 100 km. Three different datum
definition models were applied and compared, MC, OC
and WFN with distance-dependent weighting scheme.
The WFN provided the best results in terms of STD and
the mean of the time series of the fit residuals from the
known reference solution.
It should be mentioned that in the WFN approach the
observation equation system becomes undetermined
when only four satellites are visible. In this test, there
were only four visible satellites in epochs 1028-1091, and
during that time there was no solution provided.
Table 1. Absolute mean of n,e,u components derived using methods
with different constraint schemes.
The WFN approach provides the most accurate results as
compared to the MC and the OC models. The absolute
mean of the calculated rover position residuals (the
differences from the known position) equals to 3.1 cm
and 2.2 cm for east and north components respectively in
the WFN model (while e.g., MC offers 5.0 cm and 3.3
cm, respectively).
Time Series abs. Mean
[m]
Component MC OC WFN
n 0.050 0.036 0.031
e 0.033 0.028 0.023
u 0.116 0.088 0.077
Kashani et al.: Datum Definition in the Long Range Instantaneous RTK GPS Network Solution 107
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0
0.1
0.2
0.3
dn [m]
05001000 1500
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-0.2
-0.1
0
0.1
0.2
0.3
de [m]
05001000 1500
-1
-0.5
0
0.5
1
du [m]
0500 1000 1500
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
05001000 1500
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
05001000 1500
-1
-0.5
0
0.5
1
0500 1000 1500
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
05001000 1500
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
05001000 1500
-1
-0.5
0
0.5
1
Minimum
Cons traints
Over
Constrained
Weighted
Free-Net
Epochs
Epochs Epochs
Fig. 4 The derived n,e,u versus ±3σ in all the three models.
In addition to the mean and STD analyses of the time
series, a summary analysis of the fit of the WFN solution
to the true rover coordinates was performed, with a
threshold of 10 cm for the horizontal components and 20
cm for the vertical one. The results show 98-100 and 95
percent of success rate for the horizontal and the vertical
components respectively, indicating rather high level of
performance.
It was confirmed here that the WFN approach improved
the solution and made it more stable and less noisy, as
compared to the MC and OC models. The performance
level verified with the test data indicates that the current
multi-base instantaneous RTK module of the MPGPSTM
software, based on WFN approach, might be suitable for
navigation as well as for engineering/geodetic
applications. More testing, especially using real
kinematic data is needed.
In the accuracy analysis the fit residuals were tested
against ±3.0 σ (estimated standard deviation), in order to
check the reliability of the coordinate uncertainties. The
results show a very good correlation between the
residuals and the estimated STDs. As expected, the WFN
approach provided optimal accuracies, as compared to
the MC and the OC methods. According to the results,
these correlations and the fact that almost 100 percent of
the residuals lies in-between the tolerance interval reflect
the effects of the rigorous stochastic model used in the
instantaneous RTK module. The algorithm takes into
account correlation between observations within each
baseline as well as inter-baselines correlation, which
results in a realistic stochastic model of observations,
rendering the optimal solution with a realistic VCV
matrix of the parameters.
Acknowledgements
This project is supported by NOAA, National Geodetic
Survey, N/NGS (project DG133C-02-SE-0759), and SOI
- Survey of Israel (project 2002-11). Dr. Pawel Wielgosz
is supported by the Foundation for Polish Science.
The authors would like to thank Patrick M. Ernst, P.S.,
from the Ohio Division of Civil Engineering, City of
Dayton CORS, for providing Dayton station data, and
David Conner, the Ohio Geodetic Advisor, National
Geodetic Survey, NOAA, for his help in obtaining the
data.
108 Journal of Global Positioning Systems
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