SVETLANA PANASYUK
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Error Analysis was my major independent work
related to the GPS geodesy.
Since GPS analysis heavily relies on the numerous field data sets, it is very important to find out the sources of possible errors and
correctly account for them in the solution. Some of these errors are well known now and have been resolved as
input (initial) parameters into the solution or as additional unknowns. Nevertheless there are noise
characteristics in the data which are yet unresolved and distinguishable at large (more then 100 km) baselines.
Observed plate velocities are usually in order of couple cm per year, which requires a higher resolution
technique to measure the relative distance between two sites.
For my second (after the mantle convection) research topic at MIT, I carried out an error analysis for the geodetic
measurements in the Tien-Shan region of Central Asia taken during field experiments in the summers of 1992 and 1993.
This network includes a big range in length of baselines (from 270 m to 600 km) and variety of altitudes and
geometric location of sites, as well as a large number of Block-I and Block-II satellites visible simultaneously.
The data richness of the experiment allowed to carry out many computer simulated experiments and provided good
statistical results.
Below you will find a summary of the paper discussing the results:
Analyzing an error spectrum of the GPS phase measurements, I consider low and high frequency noise components
separately.
I found that long wavelength signal in the post-fit residuals can be mostly explained by insufficiently
resolved ray delay caused by heterogeneity of atmosphere, temporal as well as spatial. As I have shown,
stochastically estimated multiple atmospheric delays at zenith allow to account for daily periodical changes in
atmosphere, if they are repeated at least every two hours. I have completed the estimation of the multiple zenith
delay for the period of significant atmosphere changes: from the beginning of thunder storm to the quiet weather.
I found that actual delay can differ from single zenith estimation by 2 cm during quiet weather and be as big as
4 cm during significant changes (thunder storm). Analyzing the LC double-differenced post-fit residuals and
calculated baseline coordinates, I have shown that introduction of the multiple atmosphere delay estimation
improves the post-fits essentially, but changes the position of sites significantly, even beyond their formal
errors. I analyzed the temporal and spatial characteristics of the residual low frequency signal of the post-fits
and suggest that its source is azimuthal asymmetry of the atmosphere, which causes the delay up to 1 cm of the
rays coming from the low elevation satellites. This effect is seen as long wavelength structure of small amplitude
on the span of double differenced LC post-fits. I believe that introduction of additional stochastically estimated
parameters around the horizon at time and place of arising/sating satellites will allow to account for the error
in the solution.
I have shown that high frequency errors can be described as combination of gaussian white noise and first order
Gauss-Markov process. To recognize their statistical characteristics I completed the analysis of 643 sets of LC
double-differenced post-fit residuals and their auto-correlation functions. I believe that consistent
interpretation of the high frequency errors has to consider combination of gaussian white noise with covariance
of 5 mm and first order Gauss-Markov process with correlation time 180 sec and standard deviation 8 mm. Time
correlated noise will affect the single-day solution and covariance matrix of the coordinates as well as the
multi-day solution, which uses Kalman filter.
This research has shown many unresolved yet problems in the error interpretation of the GPS data analysis.
Although the introduction of the multiple estimation of the atmosphere delay at zenith promises to change
(probably improve) the position of stations significantly, before run new solution it will be interesting to
resolve the strange lengthening of the baselines as well as azimuthal asymmetry of the atmosphere. Also, I am
eager to see how the estimated values for relative positioning and its statistical characteristics change with
suggested adjustments in low and high frequency noise estimation; how all of these affect the global multi-session
solution, weighted and normalized rms analysis, and, finally, the estimated site velocities.
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