USING THE INTEGER DECORRELATION PROCEDURE TO INCREASE OF THE EFFICIENCY OF THE MAFA METHOD

Similar documents
Approximation of ambiguity covariance matrix for integer de-correlation procedure in single-epoch GNSS positioning

On the realistic stochastic model of GPS observables: Implementation and Performance

Influence of ambiguity precision on the success rate of GNSS integer ambiguity bootstrapping

Earth gravity field recovery using GPS, GLONASS, and SLR satellites

Statistical characteristics of L1 carrier phase observations from four low-cost GPS receivers

It is the purpose of this contribution to present the probability distribution of the 'xed' baseline. This will be done for the case the ambiguities a

IGS-related multi-gnss activities at CODE

VALIDATION OF REGIONAL GEOID MODELS FOR POLAND: LOWER SILESIA CASE STUDY

ESTIMATING THE RESIDUAL TROPOSPHERIC DELAY FOR AIRBORNE DIFFERENTIAL GPS POSITIONING (A SUMMARY)

Impact of Earth Radiation Pressure on LAGEOS Orbits and on the Global Scale

Carrier-phase Ambiguity Success Rates for Integrated GPS-Galileo Satellite Navigation

GPS cycle slips detection and repair through various signal combinations

Autocorrelation Functions in GPS Data Processing: Modeling Aspects

TREATMENT OF NUISANCE PARAMETER IN ADJUSTMENT (PHASED ADJUSTMENT)

TOWARDS ROBUST LOCALIZATION OF RTK-GPS TOPOGRAPHIC SURVEYS 23

LONG-BASELINE, SUB-DECIMETER KINEMATIC GPS POSITIONTNG OF MOVING OBJECT, WITH POTENTIAL APPLICATION TO MONITOR OCEAN SURFACE WAVE

ARTIFICIAL SATELLITES, Vol. 41, No DOI: /v

Impact of Tropospheric Delay Gradients on Total Tropospheric Delay and Precise Point Positioning

GNSS-specific local effects at the Geodetic Observatory Wettzell

TEN YEARS OF DEFORMATION STUDY AND PROPOSED RESEARCH PROGRAM FOR THE AREA OF POLISH COPPER BASIN

Design of Adaptive Filtering Algorithm for Relative Navigation

ESTIMATION OF NUTATION TERMS USING GPS

Ionosphere influence on success rate of GPS ambiguity resolution in a satellite formation flying

Global Journal of Engineering Science and Research Management

Author copy. Acta Geophysica vol. 60, no. 4, Aug. 2012, pp DOI: /s

An Improvement of Rinex-Shift Algorithm for Continuous GPS Carrier-Phase Time Transfer (Final Version).pdf

Earth gravity field recovery using GPS, GLONASS, and SLR satellites

Use of ground-based GNSS measurements in data assimilation. Reima Eresmaa Finnish Meteorological Institute

STUDIES OF DISPLACEMENTS OF GPS STATIONS ON POLISH COPPER BASIN AREA Alojzy Wasilewski 1, Zofia Rzepecka 1, Stanislaw Oszczak 2

estimator is a random vector. Conceptually we may write a = F (y), where a denotes the integer ambiguity vector, y the vector of observables, and F (:

Noise Characteristics in High Precision GPS Positioning

Performance Evaluation of Integrated GPS/GIOVE Precise Point Positioning

SIGMA-F: Variances of GPS Observations Determined by a Fuzzy System

IMPRECISION IN GEODETIC OBSERVATIONS CASE STUDY GPS MONITORING NETWORKS

ARTIFICIAL SATELLITES, Vol. 41, No DOI: /v THE LAMBDA METHOD FOR THE GNSS COMPASS

On GNSS Ambiguity Acceptance Tests

Integer carrier-phase ambiguity resolution is the key to fast. Integer Aperture Estimation. A Framework for GNSS Ambiguity Acceptance Testing

TECTONIC MOVEMENTS MONITORING OF SUDETIC MARGINAL FAULT USING SHORT GPS BASELINES

The Victorian Seismic Zone 2011 GNSS Campaign Data Analysis

Availability and Reliability Advantages of GPS/Galileo Integration

On the Spectrum of the GPS DD-Ambiguities

Reliability of the Conventional Deformation Analysis Methods for Vertical Networks

Common Realization of Terrestrial and Celestial Reference Frame

Modified Leaky LMS Algorithms Applied to Satellite Positioning

EESC Geodesy with the Global Positioning System. Class 7: Relative Positioning using Carrier-Beat Phase

Post-Processed Precise Point Positioning: A Viable Alternative?

THE EFFECT OF PHYSICAL CORRELATIONS ON THE AMBIGUITY RESOLUTION AND ACCURACY ESTIMATION IN GPS DIFFERENTIAL POSITIONING

Impact of A Priori Gradients on VLBI-Derived Terrestrial Reference Frames

Impact of A Priori Gradients on VLBI-Derived Terrestrial Reference Frames

Developments towards GNSS real-time service in GFZ

Enhancement of GPS Single Point Positioning Accuracy Using Referenced Network Stations

NATIONAL REPORT OF POLAND TO EUREF 2011

An Assessment of the Accuracy of PPP in Remote Areas in Oman

The APREF Project: First Results and Analysis

The 2008 Local-tie Survey at the Onsala Space Observatory

Improved GNSS-Based Precise Orbit Determination by using highly accurate clocks

GPS Geodesy - LAB 7. Neglecting the propagation, multipath, and receiver errors, eq.(1) becomes:

GEODYNAMICS AND DEFORMATIONS OF THE SUDETIC GEOLOGICAL STRUCTURAL BLOCKS

The APREF Project. The Asia-Pacific regional geodetic

GGSP: Realisation of the Galileo Terrestrial Reference Frame

arxiv:physics/ v1 [physics.geo-ph] 29 Jul 2004

Dealing with significant differential tectonic plate velocities within an RTK-network: The case of HEPOS

The effect of an unknown data bias in least-squares adjustment: some concerns for the estimation of geodetic parameters

Carrier Phase Techniques

EUREF Technical Note 1: Relationship and Transformation between the International and the European Terrestrial Reference Systems

Deformation Studies of the Dam of Mornos Artificial Lake via Analysis of Geodetic Data

GOCE based Gravity Field Models Signal and Error Assessment

The GOP analysis center: a global near real-time solution

Global Mapping Function (GMF): A new empirical mapping function based on numerical weather model data

Formulation of L 1 Norm Minimization in Gauss-Markov Models

Fundamental Station Wettzell - geodetic observatory -

Introduction to Least Squares Adjustment for geodetic VLBI

IS THE SUDETIC MARGINAL FAULT STILL ACTIVE? RESULTS OF THE GPS MONITORING

Evaluation of the Earth Gravity Model EGM2008 in Algeria

GPS Multipath Detection Based on Sequence of Successive-Time Double-Differences

Modern Navigation

Ephemeris Monitor for GBAS Using Multiple Baseline Antennas with Experimental Validation

A. Barbu, J. Laurent-Varin, F. Perosanz, F. Mercier and J. Marty. AVENUE project. June, 20

The GOCE Geoid in Support to Sea Level Analysis

Impact of the SRP model on CODE's 5- system orbit and clock solution for the MGEX

Evaluation of Two Integer Ambiguity Resolution Methods for Real Time GPS Positioning

Integer least-squares theory for the GNSS compass

Technical Sciences 16(4) 2013

Accelerometers for GNSS Orbit Determination

Multi-GNSS Working Group Technical Report 2016

Atmospheric delay. X, Y, Z : satellite cartesian coordinates. Z : receiver cartesian coordinates. In the vacuum the signal speed c is constant

The Global Mapping Function (GMF): A new empirical mapping function based on numerical weather model data

Evaluation of the impact of atmospheric pressure loading modeling on GNSS data analysis

MODELS OF VERTICAL MOVEMENTS OF THE EARTH CRUST SURFACE IN THE AREA OF POLAND DERIVED FROM LEVELING AND GNSS DATA

Dependences in the pillar Earth s gravity field of

INTERNATIONAL SLR SERVICE

On the use of meteo data. How to raise the value of EPN s

Delay compensated Optical Time and Frequency Distribution for Space Geodesy

Height Modernization 2013 A New Canadian Vertical Datum

Recursive Model Selection for GNSS-Combined Precise Point Positioning Algorithms

ACCURACY ASSESSMENT OF DIGITAL HEIGHT MODELS DERIVED FROM AIRBORNE SYNTHETIC APERTURE RADAR

INSAR ATMOSPHERIC DELAY MIGITIGATION BY GPS; CASE STUDY IZMIT EARTQUAKE INTERFEROGRAMS

Test Computations

Integer Least Squares: Sphere Decoding and the LLL Algorithm

GPS DESIGN: UNDIFFERENCED CARRIER BEAT PHASE OBSERVATIONS AND THE FUNDAMENTAL DIFFERENCING THEOREM

Transcription:

ARIFICIAL SAELLIES, Vol. 46, No. 3 2 DOI:.2478/v8-2-2- USING HE INEGER DECORRELAION PROCEDURE O INCREASE OF HE EFFICIENCY OF HE MAFA MEHOD S. Cellmer Institute of Geodesy University of Warmia and Mazury in Olsztyn, Olsztyn e-mail: slawomir.cellmer@uwm.edu.pl ABSRAC. he Modified Ambiguity Function Approach (MAFA) is a method of GNSS carrier phase processing. In this method, the functional model of the adjustment problem contains the conditions ensuring the "integerness" of the ambiguities. hese conditions are expressed in the form of differentiable function. A prerequisite for obtaining the correct solution is a mechanism ensuring not only the "integerness" of the ambiguity but also appropriate localization of the search space in the place where the ambiguities have correct values. One of such mechanisms is cascade adjustment, applying the linear combinations of the signals L and L2 with the integer coefficients and various wavelengths. his paper presents another, independent from the previous, approach to increase the efficiency of the MAFA method. It is based on the application of the integer decorrelation matrix to transform observation equations into equivalent, but better conditioned, observation equations. he transformation matrix is obtained in the well-known ambiguity variance-covariance matrix integer decorrelation process. Keywords:GNSS data processing, ambiguity function, MAFA method.. INRODUCION he main subject of this paper is an improved algorithm of the MAFA (Modified Ambiguity Function Approach) method, Cellmer et al. (2), Cellmer (2a), Cellmer (2b), Cellmer et al. (2). he MAFA algorithm takes into account the integer nature of the selected parameters without the necessity for the additional stage of the integer search. It is based on the Least-Squares Adjustment (LSA) algorithm with condition equations, in the functional model. In this paper, a new technique to improve the efficiency of the MAFA method is proposed. his technique exploits an integer decorrelation procedure. After transformation of the observation equations with an integer decorrelation matrix, a model of an adjustment problem turns into an equivalent model,although better conditioned. he next section presents the theoretical basis of the MAFA method. In the third section, the improvement of the efficiency using integer decorrelation procedure is proposed. he last part of the paper gives a numerical example and some conclusions. his work was supported by grant No. N N526 9937 from the Polish Ministry of Science and Higher Education.

4 2. MAFA MEHOD he following simple form of the observation equation for double differenced (DD) carrier phase observable is assumed, Hofmann-Wellenhof et.al. (28), Leick (24), eunissen (998): Φ+v= ρ X N, () λ DD carrier phase observable (in cycles) signal wave length v residual (measurement noise) X c receiver coordinate vector (X c ) DD geometrical range N integer number of cycles (DD initial ambiguity) c he nominal accuracy of the carrier phase measurement is about. cycle, Hofmann- Wellenhof et al. (28). hus, the residual values should be much lower than half a cycle. Hence, taking into account the integer nature of the ambiguity parameter N, the equation () can be rewritten in the following form: +v - round -. (2) or v round - -. (3) where round is a function of rounding to the nearest integer value. he residual (3) does not contain a term N. Nevertheless, it takes into account the integer nature of ambiguities. he right side of the equation (3) can be expressed in the form of the following, differentiable and continuous function, Cellmer and Wielgosz, (2): arcsin[sin( s)]for s s : cos( s) round(s) s (4) arcsin[sin( s)]for s s : cos( s), where s is an auxiliary variable: s -. (5) Each of the DD carrier phase observations is linearized. After linearization, the general formula of the residual equations can be shown in the following form: V= AX+, (6) with: x y z A 2 2 2 x y z n n n x y z (7) V residual vector (n ), round (8)

5 X parameter vector (increments to a prioricoordinates vector X ), A design matrix (n 3), misclosures vector (n ), he LS solution of the formula (6) is: X = - (A PA) - A P, (9) with P as the weight matrix. In order to assure the convergence of the computational process to the correct solution, different linear combinations (LC) of L and L2 GPS carrier phase observables with integer ambiguities and longer wavelengths are applied in the cascade adjustment (Jung and Enge, 2). able presents the linear combinations used in the MAFA method, along with their wavelengths (Han and Rizos 996; Cellmer et al., 2). able Linear combinations of L and L2 signals with integer ambiguity LC [m] -3L + 4L2.628 L L2.869 L.93 he above linear combinations were chosen based on the analyses of the theoretical properties of these combinations, Han and Rizos (996), Urquhart (29), Cocard and Geiger (992). he computations are performed successively for different LC in the order listed in able, namely, starting from LC with the longest wavelength and finishing with L signal only. 3. IMPROVEMEN OF HE EFFICIENCY USING HE DECORRELAION PROCEDURE he ambiguities N are usually strongly correlated. Hence, fixing one value of ambiguity through rounding value s in (5) to the nearest integer as in (2), has an impact on the rest of the ambiguities. herefore, the correlation between ambiguities should be taken into account at rounding the right side of the equation (2). he alternative way of solving this problem can be transformation of the observation equations into the equivalent form but without correlation. his method is proposed here. Let us assume that is the integer decorrelation matrix, Chang X-W et.al. (25), Glenn and Svedensen (26), Jonge and iberius (996), Liu et. al. (999), eunissen (995): Q Nz = Q N, () Q N ambiguity covariance matrix Q Nz diagonal transformed ambiguity covariance matrix. If is integer matrix then transformed ambiguity vector, N =N must be integer as well. By multiplying the equation () with, one can obtain a new equation with a new integer ambiguity vector N z :

6 V (X C ) N he free term vector is computed in this case as follows: round hus, the LS solution is obtained: with: A P X A PA A P, (), (2) (3) A = A (4) here are many various methods of finding the decorrelation matrix, Hassibi A. and Boyd S. (998), Jonge and iberius (996), Liu L.. et. al. (999), Xu PL (2). In any case, the ambiguity covariance matrix Q N is required to find the matrix. he matrix Q N can be evaluated on the basis of the system of observation equations () after linearization: V=AX+BN L, (5) L free term (observed minus computed) vector B ambiguity functional model matrix he covariance matrix of the unknown vector X =[X, N] can be presented as: C A PA A PB Q X Q XN x Q NX Q N N BPA BPB BPB BPAA PA, (6) Q BPB BPAA A PA A PB. (7) In the case of the single data, matrix B is identity and Q N computed according to formula (7), is not positive definite. It causes difficulties with the decorrelation procedure and leads to incorrect solutions. herefore, an additional coefficient k is imposed, Cellmer (2): Nk Q P kpa A PA A P. If the value of this coefficient is less than one, it simulates additional observation data (e.g. pseudoranges). It is proposed here to assume k=.99. his value was derived as optimal from tests. he positive definite matrix Q Nk is a biased estimator of the ambiguity covariance matrix. Nevertheless, it is a good approximation for the purpose of decorrelation. he formula (8) can also be used for other than single solutions. When using formula (8) in the case of multi solutions, the decorrelation process is performed separately in each. All decorrelated observation equations are arranged in the form of one observation equation system which is the basis of the LS solution. (8)

7 4. NUMERICAL EXAMPLE ha data come from campaign performed in order to monitor local deformation in open-pit mine Adamów in Central Poland. his project is managed by Dr. Radoslaw Baryla from Chair of Satellite Geodesy and Navigation of University of Warmia and Mazury in Olsztyn. Figure depicts the location of the surveys. wo GPS stations of ASG-EUPOS (Polish part of European Positioning System active geodetic network) were used in test surveys ( KONI and KUN ). he surveys were performed on December 9th, 28, on 5 km, 3 km and km baselines, with a 3-second sampling rate. Data sets of each baseline were divided into several dozen (respectively: 82, 98 and 62) 2-minute sessions (4 s). Fig. he location of the test surveys http://www.asgeupos.pl/webpg/graph/dwnld/map_pl_en.jpg he sessions were processed according to proposed approach. In each 2-minute session, the first solution was obtained from one. Further solutions were obtained on the basis of data sets subsequently increased with data from consecutive s. he decorrelation procedure was performed in each using the method derived by Liu et.al. (999). he ambiguity covariance matrix was formed according to formula (8), as a base for the decorrelation procedure. he true coordinates were derived using Bernese software on the basis of an 8 hour data set, Dach (27). Figure 2 presents the results of some selected sessions as the example from among 8 sessions of the processing of 5 km and 3 km baselines. here are linear residuals, with respect to the true position from Bernese. he residuals were computed as: 2 2 2 r dn de du, where dn, de, du are accordingly north, east and vertical components of the residuals with respect to the "true" position. baseline 5 km a) time to stable solution b) 2. linear ressidual [m] 2.,8,6,4,2.,8,6,4,2 5 5 2 25 3 35 4 linear residuals [m],8,6,4,2.,8,6,4,2 baseline 3 km time to stable solution 5 5 2 25 3 35 4

8 2.,8 c) d) linear residual [m],6,4,2.,8,6,4,2 time to stable solution 5 5 2 25 3 35 4 5 5 2 25 3 35 4 Fig. 2 he results of the baseline processing (selected examples) he blue line depicts the residuals for the solutions, while the red line represents the solutions. In case a) the solution stabilized after 2 th session whereas the solution was close to true from the first. he plot b) presents the session in which the solution gave false results whereas a good solution was obtained in the 2 th. he plots c) and d) show the examples of the results for shorter baseline: about 3 km. In the session presented in plot c) the solution stabilized after 7th, whereas the correct solution was already stabilized from the st. In the case shown in plot d) the solution was correct from st and the solution stabilized after 2th on incorrect value (7 cm from correct position). Fig. 3 shows the histograms of the correct stable solutions i.e. the frequency of stabilizing of the correct solution in a respective period of time. he frequency is expressed in [%] of the total number of the solutions. he histograms were plotted on the basis of the results from 62 sessions for km baseline, 98 sessions for 3 km baseline and 82 sessions for 5 km baseline. As we can see in the first histogram for short baselines, the number of the correct solutions stabilized in respective periods of time is similar for two variants: with and without decorrelation. However for longer baselines, in this case 3 km (the second column), the number of correct solution obtained in the starting 5 s for the variant without decorrelation amounted to 35% and for the variant almost 7 %. he impact of the decorrelation procedure is in this case significant. An even more significant impact of decorrelation procedure occurs for 5 km baselines (the third column). In the starting 5 s, over 6% correct solutions were obtained for decorrelation variant and less than 5% for the variant. In over 7% cases there were no correct solutions until the 4 th for the variant. linear residual [m] 2.,8,6,4,2.,8,6,4,2 time to stable solution % 9 8 7 6 5 4 3 2 he baselines length km 3 km 5 km % % 8 8 7 6 6 5 4 4 3 2 2-5 6- -5-5 6- -5 6-2 2-25 26-3 3-35 36-4 >4-5 6- -5 6-2 2-25 26-3 3-35 36-4 >4 Fig. 3 he histograms of the correct stable solutions

9 5. CONCLUSIONS he integer decorrelation procedure can improve the efficiency of the MAFA method. he impact of the decorrelation procedure on the efficiency of the MAFA method depends on the baseline length. A longer baseline length corresponds to a higher impact of decorrelation on the efficiency of the MAFA method. he MAFA method makes it possible to obtain good solutions from a single only. In this case, the decorrelation procedure is performed on the basis of the biased estimator of the ambiguity covariance matrix. In order to derive a form of this matrix, a new coefficient k must be applied to obtain a positive definiteness of the covariance matrix. REFERENCES Cellmer S., Wielgosz P., Rzepecka. (2) Modified ambiguity function approach for GPS carrier phase positioning. Journal of Geodesy, vol. 84, 264-275. Cellmer S. (2a) he real time precise positioning using MAFA method, he 8 th International Conference ENVIRONMENAL ENGINEERING, selected papers, vol. III, Vilnius, s.3-34 Cellmer S. (2b), A Graphic Representation of the Necessary Condition for the MAFA Method. ransactions on Geoscience and Remote Sensing, vol. PP Isssue: 99, -7. Cellmer S. and Wielgosz P. (2) GNSS Carrier Phase Processing Using Modified Ambiguity Function Approach, Florence, Italy, May 27-3 29, EUREF Publication, Mitteilungen des Bundesamtes für Kartographie und Geodäsie (Submitted for publication), on line available http://www.epncb.oma.be/_newsmails/papers/eurefsymposium29/gnss_carrier_phase_ processing_using_modified_ambiguity_function.pdf Chang X-W, Yang X, hou. (25) MLAMBDA: a modified LAMBDA method for integer least-squares estimation, Journal of Geodesy 79, 552-565. Cocard M., Bourgon S. Kamali O., Collins P. (28) A systematic investigation of optimal carrier-phase combinations for modernized triple-frequency GPS, Journal of Geodesy vol. 82, 555-564. Dach R, Hugentobler U, Fridez P, Meindl M (27) BERNESE GPS Software Version 5.. Astronomical Institute, University of Berne. Glenn J., Svedensen G. 26. Some properties of decorrelation techniques in the ambiguity space GPS Solution vol., 4-44. Hassibi A. and Boyd S. (998) Integer parameter estimation in linear models with application to GPS. IEEE rans SignallProc 46, 2938-2952 Hofmann-Wellenhof B, Lichtenegger H, Wasle E. (28) GNSS-Global Navigation Satellite Systems - GPS, GLONASS, Galileo & more. Springer-Verlag Wien. Han S, Rizos C. (996) Improving the computational efficiency of the ambiguity function algorithm. Journal of Geodesy 7, 33-34. Jonge P. de., iberius Ch. (996) he LAMBDA method for integer ambiguity estimation: implementation aspects Delft Geodetic Computing Centre LGR Series. Jung J. and Enge P. (2) Optimization of Cascade Integer Resolution with hree Civil GPS Frequencies In Proc. ION GPS 2, Salt Lake City, September Leick A. (24) GPS Satellite Surveying. 3 rd edition,john Wiley and Sons, Inc. Liu L.., Hsu H.., hu Y.., Ou J.K. (999) A new approach to GPS ambiguity decorrelation Journal of Geodesy vol. 73,478-49.

eunissen P J G. (995) he least-squares ambiguity decorrelation adjustment: a method for fast GPS integer ambiguity estimation Journal of Geodesy 7, 65-82. eunissen P J G, and Kleusberg A. (998) GPS for Geodesy, Springer Verlag, Berlin Heidelberg New York. Urquhart, L. (29) An Analysis of Multi-Frequency Carrier Phase Linear Combinations for GNSS. Senior technical report, Department of Geodesy and Geomatics Engineering echnical Report No. 263, University of New Brunswick, Fredericton, New Brunswick, Canada. Xu PL (2) Random simulation and GPS decorrelation. Journal of Geodesy 75:48 423 Received: 2-8-9, Reviewed: 2--, Accepted: 2--3.