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2\documentclass[10pt]{beamer}
3\usetheme{umbc2}
4\useinnertheme{umbcboxes}
5\setbeamercolor{umbcboxes}{bg=violet!12,fg=black}
6
7\usepackage{longtable}
8\usepackage{tabu}
9\usepackage{subeqnar}
10
11\newcommand{\ul}{\underline}
12\newcommand{\be}{\begin{equation}}
13\newcommand{\ee}{\end{equation}}
14\newcommand{\bdm}{\begin{displaymath}}
15\newcommand{\edm}{\end{displaymath}}
16\newcommand{\bea}{\begin{eqnarray}}
17\newcommand{\eea}{\end{eqnarray}}
18\newcommand{\bsea}{\begin{subeqnarray*}}
19\newcommand{\esea}{\end{subeqnarray*}}
20\newcommand{\mb}[1]{\mbox{#1}}
21\newcommand{\mc}[3]{\multicolumn{#1}{#2}{#3}}
22\newcommand{\bm}[1]{\mbox{\bf #1}}
23\newcommand{\bmm}[1]{\mbox{\boldmath$#1$\unboldmath}}
24\newcommand{\bmell}{\bmm\ell}
25\newcommand{\hateps}{\widehat{\bmm\varepsilon}}
26\newcommand{\graybox}[1]{\psboxit{box .9 setgray fill}{\fbox{#1}}}
27\newcommand{\mdeg}[1]{\mbox{$#1^{\mbox{\scriptsize o}}$}}
28\newcommand{\dd}{\mbox{\footnotesize{$\nabla \! \Delta$}}}
29\newcommand{\p}{\partial\,}
30\renewcommand{\d}{\mbox{d}}
31\newcommand{\dspfrac}{\displaystyle\frac}
32\newcommand{\nl}{\\[4mm]}
33
34\title{Processing GNSS Data in Real-Time}
35
36\author{Leo\v{s} Mervart}
37
38\institute{TU Prague}
39
40\date{Frankfurt, January 2014}
41
42% \AtBeginSection[]
43% {
44% \begin{frame}
45% \frametitle{Table of Contents}
46% \tableofcontents[currentsection]
47% \end{frame}
48% }
49
50\begin{document}
51
52%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
53
54\begin{frame}
55 \titlepage
56\end{frame}
57
58%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
59
60\begin{frame}
61\frametitle{Medieval Times of GNSS (personal memories)}
62
63\begin{description}
64\item[1991] Prof. Gerhard Beutler became the director of the Astronomical Institute, University of
65 Berne. The so-called Bernese GPS Software started to be used for (post-processing) analyzes of
66 GNSS data.
67\item[1992] LM started his PhD study at AIUB.
68\item[1992] Center for Orbit Determination in Europe (consortium of AIUB, Swisstopo, BKG, IGN, and
69 IAPG/TUM) established. Roughly at that time LM met Dr. Georg Weber for the first time.
70\item[1993] International GPS Service formally recognized by the IAG.
71\item[1994] IGS began providing GPS orbits and other products routinely (January, 1).
72\item[1995] GPS declared fully operational.
73\end{description}
74
75\end{frame}
76
77%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
78
79\begin{frame}
80\frametitle{CODE-Related Works in 1990's}
81
82\begin{itemize}
83\item The Bernese GPS Software was the primary tool for CODE analyzes (Fortran~77).
84\item IGS reference network was sparse.
85\item Real-time data transmission limited (Internet was still young, TCP/IP widely accepted 1989).
86\item CPU power of then computers was limited (VAX/VMS OS used at AIUB).
87\end{itemize}
88
89In 1990's high precision GPS analyzes were almost exclusively performed in post-processing mode.
90The typical precise application of GPS at that time was the processing of a network of static
91GPS-only receivers for the estimation of station coordinates.
92
93\end{frame}
94
95%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
96
97\begin{frame}
98\frametitle{Tempora mutantur (and maybe ``nos mutamur in illis'')}
99
100\includegraphics[width=0.7\textwidth,angle=0]{pp_vs_rt.png}
101
102\vspace*{-2cm}
103\hspace*{6cm}
104\includegraphics[width=0.4\textwidth,angle=0]{ea_ztd_21h.png}
105
106
107\end{frame}
108
109
110%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
111
112\begin{frame}
113\frametitle{O tempora! O mores!}
114
115\begin{itemize}
116\item people want more and more \ldots
117\item everybody wants everything immediately \ldots
118\item \hspace*{2cm} and, of course, free of charge \ldots
119\end{itemize}
120\vspace*{5mm}
121In GNSS-world it means:
122\begin{itemize}
123\item There are many new kinds of GNSS applications - positioning is becoming just one of many
124 purposes of GNSS usage.
125\item Many results of GNSS processing are required in real-time (or, at least, with very small
126 delay).
127\item GPS is not the only positioning system. Other GNSS are being established (for practical but
128 also for political reasons).
129\item People are used that many GNSS services are available free of charge (but the development and
130 maintenance has to be funded).
131\end{itemize}
132
133\begin{block}{But \ldots}
134\end{block}
135
136\end{frame}
137
138%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
139
140\begin{frame}
141\frametitle{Nihil novi sub sole}
142
143Each GNSS-application is based on processing code and/or phase observations
144\vspace*{-3mm}
145 \begin{eqnarray*}
146 P^i & = & \varrho^i + c\;\delta - c\;\delta^i + T^i + I^i + b_P \\
147 L^i & = & \varrho^i + c\;\delta - c\;\delta^i + T^i - I^i + b^i
148 \end{eqnarray*}
149 where
150 \begin{tabbing}
151 $P^i$, $L^i$ ~~~~~~~ \= are the code and phase measurements, \\
152 $\varrho^i$ \> is the travel distance between the satellite
153 and the receiver, \\
154 $\delta$, $\delta^i$ \> are the receiver and satellite clock errors, \\
155 $I^i$ \> is the ionospheric delay, \\
156 $T^i$ \> is the tropospheric delay, \\
157 $b_P$ \> is the code bias, and \\
158 $b^i$ \> is the phase bias (including initial
159 phase ambiguity).
160 \end{tabbing}
161Observation equations reveal what information can be gained from processing GNSS data:
162\begin{itemize}
163\item geometry (receiver positions, satellite orbits), and
164\item state of atmosphere (both dispersive and non-dispersive part)
165\end{itemize}
166The observation equations also show that, in principle, GNSS is an
167\textcolor{blue!90}{interferometric} technique -- precise results are actually always relative.
168
169\end{frame}
170
171%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
172
173\begin{frame}
174\frametitle{Challenges of Real-Time GNSS Application}
175\begin{itemize}
176\item Suitable algorithms for the parameter adjustment have to be used (filter techniques instead
177 of classical least-squares).
178\item Reliable data links have to been established (between rover station and a reference station,
179 between receivers and processing center, or between processing center and DGPS correction
180 provider).
181\item Software tools for handling real-time data (Fortran is not the best language for that).
182\item Fast CPUs.
183\end{itemize}
184
185As said above -- GNSS is an interferometric technique. Processing of a single station cannot give
186precise results. However, data of reference station(s) can be replaced by the so-called corrections
187(DGPS corrections, precise-point positioning etc.) These techniques are particularly suited for
188real-time applications because the amount of data being transferred can be considerably reduced.
189
190\end{frame}
191
192%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
193
194\begin{frame}
195\frametitle{Algorithms -- Kalman Filter}
196
197\begin{small}
198
199State vectors $\bmm{x}$ at two subsequent epochs are
200related to each other by the following linear equation:
201\bdm
202\bmm{x}(n) = \bmm{\Phi}\; \bmm{x}(n-1) + \bmm{\Gamma}\;\bmm{w}(n)~,
203\edm
204where $\Phi$ and $\Gamma$ are known matrices and {\em white noise} $\bmm{w}(n)$ is a random
205vector with the following statistical properties:
206\bsea
207E(\bmm{w}) & = & \bmm{0} \\
208E(\bmm{w}(n)\;\bmm{w}^T(m)) & = & \bmm{0} ~~ \mbox{for $m \neq n$} \\
209E(\bmm{w}(n)\;\bmm{w^T}(n)) & = & \bm{Q}_s(n) ~.
210\esea
211
212Observations $\bmm{l}(n)$ and the state vector $\bmm{x}(n)$ are related to
213each other by the linearized {\em observation equations} of form
214\bdm \label{eq:KF:obseqn}
215 \bmm{l}(n) = \bm{A}\;\bmm{x}(n) + \bmm{v}(n) ~ ,
216\edm
217where $\bm{A}$ is a known matrix (the so-called {\em first-design matrix}) and
218$\bmm{v}(n)$ is a vector of random errors with the following properties:
219\bsea\label{eq:KF:resid}
220E(\bmm{v}) & = & \bmm{0} \\
221E(\bmm{v}(n)\;\bmm{v}^T(m)) & = & \bmm{0} ~~ \mbox{for $m \neq n$} \\
222E(\bmm{v}(n)\;\bmm{v^T}(n)) & = & \bm{Q}_l(n) ~.
223\esea
224
225\end{small}
226
227\end{frame}
228
229%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
230
231\begin{frame}
232\frametitle{Classical KF Form}
233
234Minimum Mean Square Error (MMSE) estimate $\widehat{\bmm{x}}(n)$ of vector
235$\bmm{x}(n)$ meets the condition
236$E\left((\bmm{x} - \widehat{\bmm{x}})(\bmm{x} - \widehat{\bmm{x}})^T\right) =
237\mbox{min}$ and is given by
238\begin{subeqnarray}\label{eq:KF:prediction}
239 \widehat{\bmm{x}}^-(n) & = & \bmm{\Phi} \widehat{\bmm{x}}(n-1) \\
240 \bm{Q}^-(n) & = & \bmm{\Phi} \bm{Q}(n-1) \bmm{\Phi}^T +
241 \bmm{\Gamma} \bm{Q}_s(n) \bmm{\Gamma}^T
242\end{subeqnarray}
243\begin{subeqnarray}\label{eq:KF:update}
244 \widehat{\bmm{x}}(n) & = & \widehat{\bmm{x}}^-(n) +
245 \bm{K}\left(\bmm{l} -
246 \bm{A}\widehat{\bmm{x}}(n-1)\right) \\
247 \bm{Q}(n) & = & \bm{Q}^-(n) - \bm{K}\bm{A}\bm{Q}^-(n) ~,
248\end{subeqnarray}
249where
250\bdm \label{eq:KF:KandH}
251 \bm{K} = \bm{Q}^-(n)\bm{A}^T\bm{H}^{-1}, \quad
252 \bm{H} = \bm{Q}_l(n) + \bm{A}\bm{Q}^-(n)\bm{A}^T ~.
253\edm
254Equations (\ref{eq:KF:prediction}) are called {\em prediction},
255equations (\ref{eq:KF:update}) are called {\em update} step of Kalman filter.
256
257\end{frame}
258
259%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
260
261\begin{frame}
262\frametitle{Square-Root Filter} \label{sec:SRF}
263\begin{small}
264Algorithms based on equations (\ref{eq:KF:prediction}) and
265(\ref{eq:KF:update}) may suffer from numerical instabilities that are primarily
266caused by the subtraction in (\ref{eq:KF:update}b). This deficiency may be
267overcome by the so-called {\em square-root} formulation of the Kalman filter
268that is based on the so-called {\em QR-Decomposition}. Assuming the
269Cholesky decompositions
270\be \label{eq:SRF:defsym}
271 \bm{Q}(n) = \bm{S}^{T} \bm{S} , \quad
272 \bm{Q}_l(n) = \bm{S}^T_l \bm{S}_l, \quad
273 \bm{Q}^-(n) = \bm{S}^{-T}\bm{S}^-
274\ee
275we can create the following block matrix and its QR-Decomposition:
276\be \label{eq:SRF:main}
277 \left(\begin{array}{ll}
278 \bm{S}_l & \bm{0} \\
279 \bm{S}^-\bm{A}^T & \bm{S}^-
280 \end{array}\right)
281=
282 N \left(\begin{array}{cc}
283 \bm{X} & \bm{Y} \\
284 \bm{0} & \bm{Z}
285 \end{array}\right) ~ .
286\ee
287It can be easily verified that
288\bsea\label{eq:SRF:HK}
289 \bm{H} & = & \bm{X}^T\bm{X} \\
290 \bm{K}^T & = & \bm{X}^{-1}\bm{Y}\\
291 \bm{S} & = & \bm{Z} \\
292 \bm{Q}(n) & = & \bm{Z}^T\bm{Z} ~ .
293\esea
294State vector $\widehat{\bmm{x}}(n)$ is computed in a usual way using the
295equation (\ref{eq:KF:update}a).
296\end{small}
297\end{frame}
298
299%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
300
301\begin{frame}
302\frametitle{Data Transfer -- NTRIP}
303
304In order to be useful data have to be provided in a well-defined \textcolor{blue}{format}.
305RTCM (Radio Technical Commission for Maritime Services) messages are widely used for GNSS data in
306real-time.
307
308\vspace*{5mm}
309
310In addition to a format the so-called \textcolor{blue}{protocol} has to be defined. Using a given
311protocol the data user communicates with the data provider.
312
313For GNSS data, the so-called \textcolor{blue}{NTRIP} streaming protocol is used.
314\begin{itemize}
315\item NTRIP stands for Networked Transport of RTCM via Internet Protocol.
316\item NTRIP is in principle a layer on top of TCP/IP.
317\item NTRIP has been developed at BKG (together with TU Dortmund).
318\item NTRIP is capable of handling hundreds of data streams simultaneously delivering the data
319to thousands of users.
320\item NTRIP is world-wide accepted (great success of BKG).
321\end{itemize}
322
323\end{frame}
324
325%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
326
327\begin{frame}
328\frametitle{NTRIP}
329
330Efficiency of data transfer using NTRIP is achieved thanks to the GNSS Internet Radio /
331IP-Streaming architecture:
332
333\begin{center}
334\includegraphics[width=0.7\textwidth,angle=0]{ntrip.png}
335\end{center}
336
337\end{frame}
338
339%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
340
341\begin{frame}
342\frametitle{NTRIP Users}
343
344\includegraphics[width=0.5\textwidth,angle=0]{numberRegisteredUsers_1.png}
345\includegraphics[width=0.5\textwidth,angle=0]{activeClients_month_1.png}
346\begin{center}
347\includegraphics[width=0.5\textwidth,angle=0]{casterTransfer_1.png}
348\end{center}
349
350\end{frame}
351
352%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
353
354\begin{frame}
355\frametitle{BKG Ntrip Client (BNC)}
356
357An important reason why NTRIP has been widely accepted is that BKG provided high-quality public
358license software tools for its usage. One of these tools is the so-called \textcolor{blue}{BKG
359Ntrip Client}.
360
361 \begin{itemize}
362 \item BNC source consists currently of approximately 50.000 lines of code
363 \item approximately 90 \% is C++, 10 \% standard C
364 \item BNC uses a few third-party pieces of software (e.g. RTCM decoders/encoders)
365 \item BNC has a good documentation (thanks Georg Weber)
366 \end{itemize}
367
368 \begin{block}{BNC is intended to be}
369 \begin{itemize}
370 \item user-friendly
371 \item cross-platform
372 \item easily modifiable (by students, GNSS beginners)
373 \item useful (at least a little bit ...)
374 \end{itemize}
375 \end{block}
376
377 \begin{block}{BNC is not only an NTRIP client \ldots}
378 \end{block}
379
380\end{frame}
381
382%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
383
384\begin{frame}
385 \frametitle{Data QC in BNC}
386 \begin{center}
387 \includegraphics[width=0.9\textwidth,angle=0]{bnc_qc2.png}
388 \end{center}
389\end {frame}
390
391%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
392
393\begin{frame}
394 \frametitle{Data QC in BNC}
395 \begin{center}
396 \includegraphics[width=0.9\textwidth,angle=0]{bnc_qc1.png}
397 \end{center}
398\end {frame}
399
400%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
401
402\begin{frame}
403 \frametitle{Precise Point Positioning with PPP}
404 \begin{center}
405 \includegraphics[width=0.9\textwidth,angle=0]{ppp1.png}
406 \end{center}
407\end {frame}
408
409%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
410
411\begin{frame}
412\frametitle{Principles of Precise Point Positioning}
413\framesubtitle{Observation Equations}
414
415The PPP is based on the processing of the ionosphere-free linear combination of phase
416observations
417\be
418L^{ij}_3 = \varrho^{ij} - c\delta^{ij} + T^{ij} + \bar{N}^{ij}_3 ~,
419\ee
420where the ambiguity term is given by
421\be
422\bar{N}^{ij}_3 = N^{ij}_3 - l^{ij}_3
423 = \frac{c\;f_2}{f^2_1-f^2_2}\;(n^{ij}_1-n^{ij}_2) + \lambda_3\;n^{ij}_1 - l^{ij}_3
424\ee
425and (optionally) the ionosphere-free linear combination of code observations
426\be
427P^{ij}_3 = \varrho^{ij} - c\delta^{ij} + T^{ij} + p^{ij}_3 ~,
428\ee
429where the code bias $p^{ij}_3$ is the linear combination of biases
430$p^{ij}_1,p^{ij}_2$
431\end{frame}
432
433%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
434
435\begin{frame}
436\frametitle{Principles of PPP Service}
437
438Apart from the orbit corrections (will be discussed later) the server has to provide the
439value $c\delta^{ij}$. That is sufficient for a client processing phase observations only.
440
441Using the code observations on the client-side is not mandatory. After an initial convergence
442period (tens of minutes) there is almost no difference between a phase-only client and the client
443that uses also the code observations. However, correct utilization of accurate code observations
444improves the positioning results during the convergence period.
445
446Client which processes code observations either
447\begin{enumerate}
448\item has to know the value $p^{ij}_3$ (the value must be provided by the server -- the most
449 correct approach), or
450\item has to estimate terms $p^{ij}_3$, or
451\item neglect the bias (de-weight the code observations -- not fully correct).
452\end{enumerate}
453Options (2) and (3) mean that the benefit of using the code observations on the client-side (in
454addition to phase observations) is minor only.
455
456\end{frame}
457
458%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
459
460\begin{frame}
461 \frametitle{PPP Options}
462 \begin{itemize}
463 \item single station, SPP or PPP
464 \item real-time or post-processing
465 \item processing of code and phase ionosphere-free combinations, GPS,
466 Glonass, and Galileo
467 \end{itemize}
468 \begin{center}
469 \includegraphics[width=0.9\textwidth,angle=0]{ppp_opt1.png} \\[2mm]
470 \includegraphics[width=0.9\textwidth,angle=0]{ppp_opt2.png}
471 \end{center}
472\end {frame}
473
474%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
475
476\begin{frame}
477\frametitle{PPP of Moving Receiver by BNC}
478 \begin{center}
479 \includegraphics[width=0.6\textwidth,angle=0]{screenshot32.png}
480 \end{center}
481\end{frame}
482
483%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
484
485\begin{frame}
486\frametitle{PPP -- Server-Side}
487
488\includegraphics[width=0.8\textwidth,angle=0]{igs_map.png}
489
490\vspace*{-2cm}
491
492\hspace*{2cm}
493\includegraphics[width=0.8\textwidth,angle=0]{bnc_rtnet_flow.png}
494
495\end{frame}
496
497%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
498
499\begin{frame}
500\frametitle{PPP -- Server-Side}
501 \begin{center}
502 \includegraphics[width=0.9\textwidth,angle=0]{bnc_feed.png}
503 \end{center}
504\end{frame}
505
506%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
507
508\begin{frame}
509\frametitle{PPP -- Server-Side}
510 \begin{center}
511 \includegraphics[width=0.9\textwidth,angle=0]{ac_results.png}
512 \end{center}
513\end{frame}
514
515%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
516
517\begin{frame}
518\frametitle{PPP -- Server-Side}
519 \begin{center}
520 \includegraphics[width=0.9\textwidth,angle=0]{ac_results2.png}
521 \end{center}
522\end{frame}
523
524%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
525
526\begin{frame}
527 \frametitle{Combination using Kalman filtering}
528 The combination is performed in two steps
529 \begin{itemize}
530 \item[1.] The satellite clock corrections that refer to different broadcast
531 messages (different IODs) are modified in such a way that they all refer
532 to common broadcast clock value (common IOD is that of the selected
533 ``master'' analysis center).
534 \item[2.] The corrections are used as pseudo-observations for Kalman filter
535 using the following model (observation equation):
536 \begin{displaymath}
537 c_a^s = c^s + o_a + o_a^s
538 \end{displaymath}
539 where
540 \begin{tabbing}
541 $c_a^s$ ~~ \= is the clock correction for satellite s estimated by \\
542 \> the analysis center a, \\
543 $c^s$ \> is the resulting (combined) clock correction for
544 satellite s, \\
545 $o_a$ \> is the AC-specific offset
546 (common for all satellites), and \\
547 $o_a^s$ \> is the satellite and AC-specific offset.
548 \end{tabbing}
549 \end{itemize}
550 The three types of unknown parameters $c^s$, $o_a$, $o_a^s$ differ in their
551 stochastic properties: the parameters $c^s$ and $o_a$ are considered to be
552 epoch-specific while the satellite and AC-specific offset $o_a^s$ is assumed
553 to be a static parameter.
554\end{frame}
555
556%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
557
558\begin{frame}
559\frametitle{PPP -- Server-Side}
560 \begin{center}
561 \includegraphics[width=0.9\textwidth,angle=0]{combination_1.png}
562 \end{center}
563\end{frame}
564
565%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
566
567\begin{frame}
568\frametitle{PPP -- Server-Side}
569 \begin{center}
570 \includegraphics[width=0.9\textwidth,angle=0]{combination_2.png}
571 \end{center}
572\end{frame}
573
574%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
575
576\begin{frame}
577\frametitle{PPP -- Server-Side}
578 \begin{center}
579 \includegraphics[width=0.9\textwidth,angle=0]{combination_3.png}
580 \end{center}
581\end{frame}
582
583%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
584
585\begin{frame}
586\frametitle{PPP -- Server-Side}
587 \begin{center}
588 \includegraphics[width=0.9\textwidth,angle=0]{tropo1.png}
589 \end{center}
590\end{frame}
591
592%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
593
594\begin{frame}
595\frametitle{PPP -- Server-Side}
596 \begin{center}
597 \includegraphics[width=0.9\textwidth,angle=0]{tropo2.png}
598 \end{center}
599\end{frame}
600
601%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
602
603\begin{frame}
604\frametitle{PPP -- Server-Side}
605 \begin{center}
606 \includegraphics[width=0.9\textwidth,angle=0]{tropo3.png}
607 \end{center}
608\end{frame}
609
610%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
611
612\begin{frame}
613 \frametitle{Principle of our PPP-RTK Algorithm}
614 For a dual-band GPS receiver, the observation equations may read as
615 \begin{eqnarray*}
616 P^i & = & \varrho^i + c\;\delta - c\;\delta^i + T^i + b_P \\
617 L^i & = & \varrho^i + c\;\delta - c\;\delta^i + T^i + b^i
618 \end{eqnarray*}
619 where
620 \begin{tabbing}
621 $P^i$, $L^i$ ~~~~~~~ \= are the ionosphere-free code and phase measurements, \\
622 $\varrho^i$ \> is the travel distance between the satellite
623 and the receiver, \\
624 $\delta$, $\delta^i$ \> are the receiver and satellite clock errors, \\
625 $T^i$ \> is the tropospheric delay, \\
626 $b_P$ \> is the code bias, and \\
627 $b^i$ \> is the phase bias (including initial
628 phase ambiguity).
629 \end{tabbing}
630 The single-difference bias $b^{ij} = b^i - b^j$ is given by
631 \begin{displaymath}
632 b^{ij} = \displaystyle\frac{\lambda_5-\lambda_3}{2}\;(n_5^{ij} + b_5^{ij})
633 + \lambda_3\;(n_1^{ij} + b_1^{ij})
634 \end{displaymath}
635 where
636 \begin{tabbing}
637 $n_1^{ij}$, $n_5^{ij}$ ~~~~ \= are the narrow-lane and wide-lane integer ambiguities \\
638 $b_1^{ij}$ \> is the narrow-lane (receiver-independent) SD bias \\
639 $b_5^{ij}$ \> is the wide-lane (receiver-independent) SD bias
640 \end{tabbing}
641\end{frame}
642
643%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
644
645\begin{frame}
646 \frametitle{Principle of our PPP-RTK Algorithm (cont.)}
647 Receiver-independent single-difference biases $b_1^{ij}$ and $b_5^{ij}$ have
648 to be estimated on the server-side.
649 \begin{itemize}
650 \item Narrow-lane bias $b_1^{ij}$ may be combined with satellite clock
651 corrections $\Longrightarrow$ \textbf{modified satellite clock corrections.}
652 \item Wide-lane bias have to be transmitted from the server to the client
653 (this bias is stable in time and can thus be transmitted in lower rate).
654 \end{itemize}
655
656 On the client-side the biases $b_1^{ij}$ and $b_5^{ij}$ are used as known
657 quantities. It allows fixing the integer ambiguities $n_5^{ij}$ and
658 $n_1^{ij}$. The technique is called Precise Point Positioning with Ambiguity
659 Resolution (PPP~AR) or PPP~RTK, or zero-difference ambiguity
660 fixing (the latter term not fully correct because the ambiguities are
661 actually being fixed on single-difference level).
662\end{frame}
663
664%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
665
666\begin{frame}
667 \frametitle{Performance}
668 \begin{center}
669 \includegraphics[width=0.75\textwidth]{kir0.png}
670 \end{center}
671 \vspace*{-5mm}
672 \begin{block}{Standard deviations (N,E,U)}
673 \vspace*{3mm}
674 \begin{small}
675 \hspace*{2cm}
676 \begin{tabular}{l|ccc|ccc}
677 \mbox{} & \multicolumn{3}{c|}{10-60 min} & \multicolumn{3}{c}{30-60 min} \\
678 float & 0.034 & 0.026 & 0.026 & 0.010 & 0.009 & 0.011 \\
679 fix & 0.007 & 0.003 & 0.016 & 0.007 & 0.003 & 0.012
680 \end{tabular}
681 \end{small}
682 \end{block}
683\end{frame}
684
685%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
686
687\begin{frame}
688 \frametitle{Challenges}
689 PPP~RTK works and provides mm-accuracy results, what is this symposium
690 about?
691
692 \pause
693 There are still both principal and technical problems and challenges:
694 \begin{itemize}
695 \item Principal problems:
696 \begin{itemize}
697 \item Convergence time: PPP~RTK in the form outlined above provides
698 accuracy similar (or even slightly better) to RTK but the convergence
699 time is longer.
700 \item There is a degradation in accuracy with the age of corrections.
701 \item Glonass ambiguity resolution: is it possible to resolve Glonass
702 ambiguities? (yes, it is possible but it implicates introducing new
703 parameters - does it really improve the results?)
704 \item ...
705 \end{itemize}
706 \item Technical problems:
707 \begin{itemize}
708 \item Availability of data in real time (reference network, high-precision
709 satellite orbits).
710 \item Very high CPU requirements on the server-side.
711 \item Solution robustness on the server-side
712 (problems with reliable DD ambiguity resolution).
713 \item ...
714 \end{itemize}
715 \end{itemize}
716\end{frame}
717
718%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
719
720\begin{frame}
721 \frametitle{Challenges (cont.)}
722 \begin{block}{Longer convergence time}
723 In case of a standard RTK the very short convergence time is being achieved
724 thanks to the combined DD ambiguity resolution on both $L_1$ and $L_2$ when
725 the differential ionospheric bias can either be neglected (short baselines)
726 or its influence is mitigated (stochastic ionosphere estimation with
727 constraints).
728
729 On the contrary, the outlined PPP~RTK algorithm is in principle based on
730 processing single (ionosphere-free) linear combination and resolving only
731 one set of (narrow-lane) initial phase ambiguities.
732 \end{block}
733 \begin{block}{Possible solutions}
734 \begin{itemize}
735 \item third carrier
736 \item multiple GNSS (Glonass ambiguity resolution?)
737 \item processing original carriers (instead of ionosphere-free linear
738 combination) and modeling the ionosphere?
739 \item ?
740 \end{itemize}
741 \end{block}
742\end{frame}
743
744%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
745
746\begin{frame}
747 \frametitle{Challenges (cont.)}
748 \begin{block}{Age of corrections 0 s}
749 \begin{center}
750 \includegraphics[width=0.6\textwidth]{age1.png}
751 \end{center}
752 \end{block}
753\end{frame}
754
755%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
756
757\begin{frame}
758 \frametitle{Challenges (cont.)}
759 \begin{block}{Age of corrections up to 35 s}
760 \begin{center}
761 \includegraphics[width=0.6\textwidth]{age2.png}
762 \end{center}
763 \end{block}
764\end{frame}
765
766%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
767
768\begin{frame}
769 \frametitle{Real-Time Data Availability}
770 \framesubtitle{IGS network: very good global coverage:}
771 \vspace*{-5.5cm}
772 \begin{center}
773 \includegraphics[width=0.9\textwidth]{map.pdf}
774 \end{center}
775\end{frame}
776
777%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
778
779\begin{frame}
780 \frametitle{Real-Time Data Availability (cont.)}
781 \begin{tabular}{cc}
782 \includegraphics[width=0.4\textwidth]{100A_lat.png} &
783 \includegraphics[width=0.4\textwidth]{101A_lat.png} \\
784 \includegraphics[width=0.4\textwidth]{102A_lat.png} &
785 \includegraphics[width=0.4\textwidth]{104A_lat.png}
786 \end{tabular}
787
788 Gaps in reference network data may degrade the PPP~RTK server performance
789 considerably!
790\end{frame}
791
792%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
793
794\begin{frame}
795 \frametitle{Technical issues}
796 \begin{block}{CPU-requirements on the server-side}
797 Processing a global reference network is a very CPU-intensive
798 task. Numerically stable forms of the Kalman filter (square-root, UDU
799 factorization etc.) require very fast hardware.
800
801 Possible solutions:
802 \begin{itemize}
803 \item Processing optimization (estimating various kinds of parameters in
804 different rates)
805 \item Parallel processing
806 \item Advanced hardware (GPS Solutions uses GPU-accelerated library)
807 \end{itemize}
808 \end{block}
809 \begin{block}{Reliable DD ambiguity resolution on the server-side}
810 Reliable double-difference ambiguity resolution on the server-side remains
811 the crucial issue of the PPP~RTK technique.
812 \end{block}
813 \begin{block}{Dissemination of PPP~RTK corrections}
814 \begin{itemize}
815 \item data links
816 \item formats (standardization?)
817 \item optimization of correction rates (bandwidth)
818 \end{itemize}
819 \end{block}
820\end{frame}
821
822%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
823
824\begin{frame}
825 \frametitle{Satellite orbits}
826
827 Predicted part of the IGS ultra-rapid orbits (available in real-time) is
828 sometimes not sufficient for the processing of a global reference network
829 (with narrow-lane ambiguity resolution). We have been forced to implement
830 the real-time orbit determination capability in our main processing tool
831 RTNet (Real-Time Network software).
832 \begin{center}
833 \includegraphics[width=0.75\textwidth]{rtnet_pod.png}
834 \end{center}
835\end{frame}
836
837%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
838
839\begin{frame}
840 \frametitle{Regional versus global PPP~RTK services}
841 Currently we are routinely running both regional and global PPP~RTK service
842 demonstrators in real-time (some of the results will be shown below).
843 \begin{itemize}
844 \item in principal there is no difference between a global and regional
845 service as far as the data processing, algorithms etc. is concerned
846 \item global PPP~RTK service has at least the following two advantages
847 \begin{itemize}
848 \item[1.] a single correction stream can serve all users
849 \item[2.] all satellites are tracked permanently (helps ambiguity
850 resolution)
851 \end{itemize}
852 \item global PPP~RTK service is much more challenging (data availability,
853 CPU-requirements on the server-side, DD ambiguity resolution on long
854 baselines, the highest requirements for the accuracy of the satellite
855 orbits)
856 \end{itemize}
857
858\end{frame}
859
860%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
861
862\begin{frame}
863 \frametitle{Services monitoring}
864 Reliable, production-quality PPP~RTK service requires sophisticated
865 monitoring tools.
866 \begin{tabular}{cc}
867 \includegraphics[width=0.6\textwidth]{monitor1.png} & \\[-1.5cm]
868 & \hspace*{-3cm} \includegraphics[width=0.6\textwidth]{monitor2.png}
869 \end{tabular}
870
871\end{frame}
872
873%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
874
875\begin{frame}
876 \frametitle{Results}
877 \begin{center}
878 \includegraphics[width=0.9\textwidth]{tsunami.pdf}
879 \end{center}
880\end{frame}
881
882%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
883
884\begin{frame}
885 \frametitle{Results (cont.)}
886 \begin{center}
887 \includegraphics[width=0.9\textwidth]{nrcan.png}
888 \end{center}
889\end{frame}
890
891\end{document}
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