11/19/01UTexas Austin Seminar1 “Global” Global Positioning System Measurements Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences.

Slides:



Advertisements
Similar presentations
Introduction to the Global Positioning System
Advertisements

Where do precise orbits and clocks come from? Kristine M. Larson ASEN 6090 Spring 2010.
GPS Theory and applications
Modern Navigation Thomas Herring MW 11:00-12:30 Room A
Principles of the Global Positioning System Lecture 19 Prof. Thomas Herring Room A;
Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology 77 Massachusetts Avenue | A | Cambridge MA V F.
04/22/02EGS G STABILITY OF GLOBAL GEODETIC RESULTS Prof. Thomas Herring Room ;
Space Weather influence on satellite based navigation and precise positioning R. Warnant, S. Lejeune, M. Bavier Royal Observatory of Belgium Avenue Circulaire,
Background Accessibility Popularity of GPS and INS –Cell phones Apple iPhone, Blackberry, Android platform –Nintendo Wii Wii Remote, MotionPlus.
GTECH 201 Session 08 GPS.
Principles of the Global Positioning System Lecture 14 Prof. Thomas Herring Room A;
GPS Satellites Satellite-based navigation system originally developed for military purposes (NAVSTAR ). NAVSTAR Global Positioning System (GPS) Globally.
Algorithms behind Global Positioning Murray Grace Josh Collins.
Introduction to the Global Positioning System. What is the GPS? Orbiting navigational satellites Orbiting navigational satellites Transmit position and.
Patrick Caldwell Chris Kellar. Overview  Basic Concepts  History  Structure  Applications  Communication  Typical Sources of Error.
GPS Global Positioning System Lecture 11. What is GPS?  The Global Positioning System.  A system designed to accurately determining positions on the.
EE 570: Location and Navigation: Theory & Practice The Global Positioning System (GPS) Thursday 11 April 2013 NMT EE 570: Location and Navigation: Theory.
July 17, 2002Zambia GNSS Earth Science Global Navigation Satellite Systems (GNSS) for Earth Sciences Prof. Thomas Herring, Massachusetts Institute.
Modern Navigation Thomas Herring
Geographic Information Systems
How Global Positioning Devices (GPS) work
Modern Navigation Thomas Herring MW 11:00-12:30 Room
Róbert Adam.  GLONASS = Global navigation satellite system (Globalnaya Navigatsionnaya Sputnikovaya Sistema)  Radio-based satellite navigation operated.
1/28/2010PRRMEC What is GPS… The Global Positioning System (GPS) is a U.S. space- based global navigation satellite system. It provides reliable positioning,
Modern Navigation Thomas Herring MW 11:00-12:30 Room
SVY 207: Lecture 4 GPS Description and Signal Structure
Esci 203, Earth Structure and Deformation Introduction to the global positioning system (GPS) John Townend EQC Fellow in Seismic Studies
Modern Navigation Thomas Herring MW 11:00-12:30 Room A
NGS GPS ORBIT DETERMINATION Positioning America for the Future NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION National Ocean Service National Geodetic.
Chapter 8: The future geodetic reference frames Thomas Herring, Hans-Peter Plag, Jim Ray, Zuheir Altamimi.
GPS: Global Positioning System  The Geographer’s best friend!  You can say with confidence… “I’m not lost!, I’m never lost!”* *Of course, where everybody.
How Does GPS Work ?. Objectives To Describe: The 3 components of the Global Positioning System How position is obtaining from a radio timing signal Obtaining.
GPS(Global Positioning System) -An Introduction. What is the GPS? Orbiting navigational satellites Transmit position and time data Handheld receivers.
Lecturer: Jinglin Wang Student name: Hao Li Student ID:
Global Positioning System
West Hills College Farm of the Future. West Hills College Farm of the Future GLONASS Russia’s global satellite navigation system 24 satellites in three.
By Andrew Y.T. Kudowor, Ph.D. Lecture Presented at San Jacinto College.
NAVSTAR GPS Mike Mickelson KD8DZ 08 Dec GPS BASICS.
GPS: “Where goeth thou” Thomas Herring With results from Jen Alltop: Geosystems Thesis Katy Quinn: Almost graduated Ph.D
SNARF: Theory and Practice, and Implications Thomas Herring Department of Earth Atmospheric and Planetary Sciences, MIT
CRGIS Global Positioning Systems The Basics CRGIS National Park Service.
GPS: Everything you wanted to know, but were afraid to ask Andria Bilich National Geodetic Survey.
GPS Global Positioning System. What is GPS?  The Global Positioning System.  A system designed to accurately determining positions on the earth  The.
Global Positioning System Overview
The Global Positioning System. Early Satellite Systems Satellite Surveying started more than 30 years ago. Now, High accuracy could be achieved in real.
Applications of the Global Positioning System Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences Seminar Fall 2004.
West Hills College Farm of the Future. West Hills College Farm of the Future Precision Agriculture – Lesson 2 What is GPS? Global Positioning System Operated.
Chapter 2 GPS Crop Science 6 Fall 2004 October 22, 2004.
EE 495 Modern Navigation Systems
1 SVY 207: Lecture 12 Modes of GPS Positioning Aim of this lecture: –To review and compare methods of static positioning, and introduce methods for kinematic.
5/18/2994G21D-04 Spring AGU Realization of a Stable North America Reference Frame Thomas Herring Department of Earth Atmospheric and Planetary, Sciences,
Principles of the Global Positioning System Lecture 09 Prof. Thomas Herring Room A;
Principles of the Global Positioning System Lecture 08 Prof. Thomas Herring Room ;
12/12/01Fall AGU Vertical Reference Frames for Sea Level Monitoring Thomas Herring Department of Earth, Atmosphere and Planetary Sciences
Aug 6, 2002APSG Irkutsk Contemporary Horizontal and Vertical Deformation of the Tien Shan Thomas Herring, Bradford H. Hager, Brendan Meade, Massachusetts.
01/05/ IAP Class Field Geophysics Instructors Tom Herring, Brad Hager Web:
Revised 10/30/20061 Overview of GPS FORT 130 Forest Mapping Systems.
The Global Positioning System Rebecca C. Smyth April 17 - May 2, 2001.
A GADGET WHICH CHANGED THE WAY THE WORLD OPERATES Global Positioning System Seminar by: B V Aparna ECE CMR College of Engg. And Tech.
Younis H. Karim, AbidYahya School of Computer University Malaysia Perlis 1.
Geodesy & Crustal Deformation
EE 495 Modern Navigation Systems
Satellite Communications
Global Positioning System Supplemental from JD Text
Geodesy & Crustal Deformation
Assessing the Compatibility of Microwave Geodetic Systems
Field Geophysics Instructors Tom Herring, Brad Hager Web:
Principles of the Global Positioning System Lecture 14
Lec 04: Introduction to GPS
Presentation transcript:

11/19/01UTexas Austin Seminar1 “Global” Global Positioning System Measurements Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences

11/19/01UTexas Austin Seminar2 Overview Review of the development of the GPS system and basics of its use and operation Selected regional applications Character of global measurements Origin of systematic effects in global results

11/19/01UTexas Austin Seminar3 GPS Original Design Started development in the late 1960s as NAVY/USAF project to replace Doppler positioning system Aim: Real-time positioning to < 10 meters, capable of being used on fast moving vehicles. Limit civilian (“non-authorized”) users to 100 meter positioning.

11/19/01UTexas Austin Seminar4 GPS Design Innovations: –Use multiple satellites (originally 21, now ~28) –All satellites transmit at same frequency –Signals encoded with unique “bi-phase, quadrature code” generated by pseudo-random sequence (designated by PRN, PR number): Spread-spectrum transmission. –Dual frequency band transmission: L1 ~1.575 GHz, L2 ~1.227 GHz Corresponding wavelengths are 190 mm and 244 mm

11/19/01UTexas Austin Seminar5 Latest Block IIR satellite (1,100 kg) ° Transmission array is made up of 12 helical antenna in two rings of 43.8 cm (8 antennas) and 16,2 cm (4 antennas) radii ° Total diameter is 87 cm ° Solar panels lead to large solar radiation pressure effects.

11/19/01UTexas Austin Seminar6 Measurements Measurements: –Time difference between signal transmission from satellite and its arrival at ground station (called “pseudo-range”, precise to 0.1–10 m) –Carrier phase difference between transmitter and receiver (precise to a few millimeters) but initial values unknown (ie., measures change in range to satellites). –In some case, the integer values of the initial phase ambiguities can be determined (bias fixing) All measurements relative to “clocks” in ground receiver and satellites (potentially poses problems).

11/19/01UTexas Austin Seminar7 Measurement usage “Spread-spectrum” transmission: Multiple satellites can be measured at same time. Since measurements can be made at same time, ground receiver clock error can be determined (along with position). Signal

11/19/01UTexas Austin Seminar8 Measurements Since the C(t) code changes the sign of the signal, satellite can be only be detected if the code is known (PRN code) Multiple satellites can be separated by “correlating” with different codes (only the correct code will produce a signal) The time delay of the code is the pseudo- range measurement.

11/19/01UTexas Austin Seminar9 Position Determination (perfect clocks). Three satellites are needed for 3-D position with perfect clocks. Two satellites are OK if height is known)

11/19/01UTexas Austin Seminar10 Position determination: with clock errors: 2-D case Receiver clock is fast in this case, so all pseudo-ranges are short

11/19/01UTexas Austin Seminar11 Positioning For pseudo-range to be used for positioning need: –Knowledge of errors in satellite clocks –Knowledge of positions of satellites This information is transmitted by satellite in “broadcast ephemeris” “Differential” positioning (DGPS) eliminates need for accurate satellite clock knowledge.

11/19/01UTexas Austin Seminar12 GPS Security systems Selective availability (SA) is no longer active but prior to 2000 “denied” civilian accuracy better than 100 m Antispoofing (AS) active since 1992, adds additional encryption to P-code on L1 and L2. Makes civilian GPS receivers more expensive and more sensitive to radio interference Impact of AS and SA small on results presented here.

11/19/01UTexas Austin Seminar13 Satellite constellation Since multiple satellites need to be seen at same time (four or more): –Many satellites (original 21 but now 28) –High altitude so that large portion of Earth can be seen (20,000 km altitude —MEO)

11/19/01UTexas Austin Seminar14 Current constellation Relative sizes correct (inertial space view) “Fuzzy” lines not due to orbit perturbations, but due to satellites being in 6-planes at 55 o inclination.

11/19/01UTexas Austin Seminar15 Global GPS analysis GPS phase measurements at L1 and L2 from a global distribution of station used Analysis here is “un-constrained” –All site positions estimated –Atmospheric delay parameters estimated –“Real” bias parameters for each satellite global, integer values for regional site combinations (<500 km) –Orbital parameters for all satellites estimated (1-day orbits, 2-revolutions) 6 Integration constants 3 constant radiation parameters 6 once-per-revolution radiation parameters

11/19/01UTexas Austin Seminar16 Global GPS analysis Data used between Full analysis has ~600 stations (analysis here restricted to ~100 sites that have more than 5 years of data Large density of sites (~300) in California Total data set has > 2 billion phase measurements

11/19/01UTexas Austin Seminar17 GPS Antennas (for precise positioning) Rings are called choke-rings (used to suppress multi-path) Nearly all antennas are patch antennas (conducting patch mounted in insulating ceramic).

11/19/01UTexas Austin Seminar18 Global IGS Network (~150 stations)

11/19/01UTexas Austin Seminar19 Specific sites analyzed Total of 100 sites analyzed of which 50 were used to realize coordinate system Since analysis has little constraint, it is: –Free to rotate –Possibly free to translate (explicit estimation) –Possibly free to change scale (explicit estimation) Latter too effects should not be present but these we will explore here.

11/19/01UTexas Austin Seminar20 Network used in analysis Black: Frame sites; Red other sites

11/19/01UTexas Austin Seminar21 Results from analysis Examples of time series for some sites –“Common Mode” error, example of regional frame definition Satellite phase center positions Scale and Center of Mass (CoM) variations

11/19/01UTexas Austin Seminar22 Example of motions measured in Pacific/Asia region Fastest motions are >100 mm/yr Note convergence near Japan More at

11/19/01UTexas Austin Seminar23 California East residuals (trends removed)

11/19/01UTexas Austin Seminar24 East position residuals (California)

11/19/01UTexas Austin Seminar25 Example from “regional” frame definition

11/19/01UTexas Austin Seminar26 “Desert” California site

11/19/01UTexas Austin Seminar27 Origin of “common” mode errors Unknown at the moment, but clearly scales with distance (172 of 500 sites in S.California have sub-mm daily horizontal scatter, 2-3 mm vertical) Possible effects from satellite transmission system. Example of estimating corrections to phase center position (wrt CoM) of satellites

11/19/01UTexas Austin Seminar28 Phase center offsets  = dh cos  ; sin  = (R/a) sin  ; (R/a) = 0.24

11/19/01UTexas Austin Seminar29 Elevation angle dependence

11/19/01UTexas Austin Seminar30 Full estimation effects

11/19/01UTexas Austin Seminar31 Effects of phase center position changes A unit change in the radial phase center position will change the range to the satellite by a constant plus up to 0.03 units. For 1 meter change; range change about 5 parts-per-billion If different models of satellites have difference phase center positions, scale could change with time.

Total phase center position and adjustment to specified values

11/19/01UTexas Austin Seminar33 Scale variations with time

11/19/01UTexas Austin Seminar34 Center of mass variations as well

11/19/01UTexas Austin Seminar35 Conclusion Regional GPS (e.g., California) yields sub- millimeter results for “good” stations Globally RMS increase to 2-3 mm for reasons that are not clear Secular scale change -1.6 mm/yr in height (Reference sites have 0.8 mm/yr average) In GAMIT: -120 mm Z-offset in CoM for unknown reasons Differences between generations of satellites might explain some of these results. Systematic nature suggests we might be able to resolve

11/19/01UTexas Austin Seminar36 Relativistic Corrections terms Propagation path curvature due to Earth’s potential (a few centimeters) Clock effects due to changing potential For e=0.02 effect is 47 ns (14 m)

11/19/01UTexas Austin Seminar37 Relativistic Effects

11/19/01UTexas Austin Seminar38 Tectonic Deformation Results “Fixed GPS” stations operate continuously and by determining their positions each day we can monitor their motions relative to a global coordinate system Temporary GPS sites can be deployed on well defined marks in the Earth and the motions of these sites can be monitored (campaign GPS)

11/19/01UTexas Austin Seminar39 Locations measured with GPS Red are campaign (~5000), other colors continuous GPS operated by different groups

11/19/01UTexas Austin Seminar40 Motion in North America Note rapid change in California Remainder of field consistent with rotating NA plate

11/19/01UTexas Austin Seminar41 Detail in Western United States

11/19/01UTexas Austin Seminar42 California Detail Compilation of continuous and campaign GPS Only  <1.5 mm/yr shown In 100 years, fastest points move 5 m

11/19/01UTexas Austin Seminar43 Motion in Turkey and Aegean

11/19/01UTexas Austin Seminar Izmit Earthquake Black vectors are observed, Yellow model calculation

11/19/01UTexas Austin Seminar45 Motion after Earthquakes. Example from Hector Mine, CA Continued motion tells us about material characteristics and how stress is re-distributed after earthquake

11/19/01UTexas Austin Seminar46 Other applications Aircraft positioning, vehicle navigation, engineering (real-time differential GPS links shown)

11/19/01UTexas Austin Seminar47 Relativistic effects General relativity affects GPS in three ways –Equations of motions of satellite –Rates at which clock run –Signal propagation In our GPS analysis we account for the second two items Orbits only integrated for 1-3 days and equation of motion term is considered small

11/19/01UTexas Austin Seminar48 Clock effects GPS is controlled by MHz oscillators On the Earth’s surface these oscillators are set to 10.23x( x ) MHz (39,000 ns/day rate difference) This offset accounts for the change in potential and average velocity once the satellite is launched. The first GPS satellites had a switch to turn this effect on. They were launched with “Newtonian” clocks

11/19/01UTexas Austin Seminar49 Propagation and clock effects Our theoretical delay calculations are made in an Earth centered, non-rotating frame using a “light-time” iteration i.e., the satellite position at transmit time is differenced from ground station position at receive time. Two corrections are then applied to this calculation

11/19/01UTexas Austin Seminar50 Effects of Selective Availability

11/19/01UTexas Austin Seminar51 Conclusions GPS dual-use technology: Applications in civilian world widespread –Geophysical studies (mm accuracy) –Engineering positioning (<cm in real-time) –Commercial positioning: cars, aircraft, boats (cm to m level in real-time) Relativistic effects are large but largely constant However due to varying potentials and velocities effects can be seen Some effects are incorporated by convention Need to keep in mind “negligible effects” as accuracy improves