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Slajd 1

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Title: Slajd 1


1
Real-time Kinematic GPS Positioning Supported by
Predicted Ionosphere Model
P. Wielgosz and A. Krankowski
University of Warmia and Mazury in Olsztyn,
Poland pawel.wielgosz_at_uwm.edu.pl
IGS AC Workshop Miami Beach, June 2-6, 2008
2
Outline
  • Research objectives
  • ARMA method
  • RTK positioning model
  • Experiment design
  • Test results and analysis
  • Conclusion

3
Research Objectives
  • Develop and evaluate methodology and algorithms
    for OTF-RTK positioning technique suitable for
    medium and long ranges 10-100 km
  • Test applicability of predicted ionosphere models
    to support medium range OTF-RTK positioning
  • Evaluate prediction model based on ARMA method
  • Study the impact of the model accuracy on the
    ambiguity resolution (speed and reliability)

4
Methodology ARMA prediction of real-valued time
series
Let yt for t 1, 2, . , n be an equidistant
stationary stochastic time series and yt1 be
the prediction at time t1. The
autoregressive-moving average process ARMA(p,q)
is defined by the formula where ?i are
autoregressive coefficients, ?i are the moving
average coefficients,p and q are the
autoregressive and moving average orders, ?i is a
white noise process After introducing the
backshift operator BK the process can be
converted to
5
Methodology ARMA prediction of real-valued time
series
The ARMA forecast L steps ahead
- the part of the operator containing only
nonnegative powers of B
10 previous days of the TEC values were taken
for the prediction computation
6
Methodology ARMA prediction of real-valued time
series
  • Our previous studies showed that the TEC
    prediction for 1- to 3 hours ahead yields values
    very close to real, observed TEC (under quiet to
    moderate geomagnetic conditions)
  • After 3 hours the quality of the forecast
    diminishes very quickly
  • ARMA forecasting method is very simple and does
    not need any a-priori information about the
    process nor additional inputs such as, e.g.,
    solar or geomagnetic activity indices

Reference Krankowski A., Kosek W., Baran
L.W., Popinski W., 2005, Wavelet analysis and
forecasting of VTEC obtained with GPS
observations over European latitudes, Journal of
Atmospheric and Solar-Terrestrial Physics, 67
(2005), pp. 1147 1156
7
Methodology ARMA prediction of real-valued time
series
  • GPS data from European IGS stations were used for
    TEC calculations
  • 10 previous days of the TEC values were taken for
    the prediction computation
  • Prediction for May 8, 2007
  • Ionospheric conditions with max Kp4o and sum of
    Kp 22

http//igscb.jpl.nasa.gov
Test network area
8
Methodology Positioning Adjustment Model
Sequential Generalized Least Squares (GLS)
  • All parameters in the mathematical model are
    considered pseudo-observations with a priori
    information (s 0 ?)
  • Two characteristic groups of interest

- instantaneous parameters (e.g., DD ionospheric
delays)- accumulated parameters (e.g., DD
ambiguities)
  • Flexibility, easy implementation of
  • stochastic constraints
  • fixed constraints
  • weighted parameters

9
Methodology Positioning
  • MPGPS software was used for all calculations
  • Mathematical model uses dual-frequency code and
    phase GPS data
  • Unknowns DD Ionospheric delays, Tropospheric TZD
    per station, DD ambiguities, rover coordinates
  • Tropospheric TZD calculated at the reference
    stations and interpolated to the rover location,
    tightly constrained in GLS
  • DD Ionospheric delays obtained from the ARMA
    forecast, constrained to 10-20 cm in GLS
  • Ambiguity resolution Least square AMBiguity
    Decorrelation Algorithm (LAMBDA)
  • Validation W-test - minimum of 3 observational
    epochs (for 5-second sampling rate) and W-test gt
    4 required for validation

10
Experiment
  • GPS data from ASG-EUPOS and EPN networks
  • 24-hour data set collected on May 8, 2007 with
    5-second sampling rate
  • KATO station selected as a simulated user
    receiver (rover)
  • Ambiguity resolution was restarted every 5
    minutes (288 times)
  • Maximum 5 minutes (60 epochs) for initialization
    allowed

25 km
67 km
50 km
Map www.asg-pl.pl
11
Experiment
  • 3 baselines of different length were processed
    independently (single baseline mode) and also in
    a multi-baseline mode (all baselines together)
  • predicted iono model was applied (1-2 hour
    forecast)
  • Time-to-fix was analyzed
  • Ambiguity resolution success rate was analyzed
  • Ambiguity validation failure ratio was analyzed
  • True reference coordinates derived using
    Bernese software
  • IGS predicted orbits and clocks used (ultra-rapid)

25 km
67 km
50 km
Map www.asg-pl.pl
12
Test results
DD Ionospheric correction residuals, KATO-TARG
baseline 25 km
13
Test results
DD Ionospheric correction residuals, KATO-WODZ
baseline 50 km
14
Test results
DD Ionospheric correction residuals, KATO-KRAW
baseline 67 km
15
Test results
Kinematic position residuals (NEU), KATO-TARG
baseline 25 km
16
Test results
Kinematic position residuals (NEU), KATO-WODZ
baseline 50 km
17
Test results
Kinematic position residuals (NEU), KATO-KRAW
baseline 67 km
18
Test results
Kinematic position residuals (NEU),
multi-baseline 25, 50 and 67 km
19
Test results and analysis
Ambiguity resolution statistics
minimum 3 epochs (15 seconds) required for
validation
20
Conclusions
  • Cm-level horizontal kinematic position accuracy
    can be achieved using proposed methodology with
    dual-frequency GPS data over distances of tens of
    km
  • When the ionospheric correction accuracy is
    better that ½ cycle of L1 signal, fixed solution
    is possible just after a few observational epochs
    only
  • The ionosphere forecast model reduce 40 of the
    ionospheric delay (its accuracy is limited by the
    base model)
  • The applicability of the presented forecast model
    is limited to the distances of 25-50 km in a
    single-baseline mode and to 60-70 km in a
    multi-baseline mode

21
Future Developments
  • Research on the level of stochastic constraints
    imposed on the ionospheric corrections
  • Too tight constraints cause false fixes
  • Too loose constraints make time-to-fix longer
  • Test prediction of more accurate ionospheric
    (base) models
  • Higher accuracy base models will also improve
    accuracy of the prediction, and hence, the
    predicted TEC level will be more beneficial to
    RTK positioning
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