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

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Presentation on theme: "11/19/01UTexas Austin Seminar1 “Global” Global Positioning System Measurements Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences."— Presentation transcript:

1 11/19/01UTexas Austin Seminar1 “Global” Global Positioning System Measurements Prof. Thomas Herring Department of Earth, Atmosphere and Planetary Sciences http://www-gpsg.mit.edu/~tah

2 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

3 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.

4 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

5 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.

6 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).

7 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

8 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.

9 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)

10 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 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.

12 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.

13 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)

14 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.

15 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

16 11/19/01UTexas Austin Seminar16 Global GPS analysis Data used between 1992-2001 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

17 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).

18 11/19/01UTexas Austin Seminar18 Global IGS Network (~150 stations)

19 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.

20 11/19/01UTexas Austin Seminar20 Network used in analysis Black: Frame sites; Red other sites

21 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

22 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 http://www-gpsg.mit.edu/~fresh/index2.htmlhttp://www-gpsg.mit.edu/~fresh/index2.html

23 11/19/01UTexas Austin Seminar23 California East residuals (trends removed)

24 11/19/01UTexas Austin Seminar24 East position residuals (California)

25 11/19/01UTexas Austin Seminar25 Example from “regional” frame definition

26 11/19/01UTexas Austin Seminar26 “Desert” California site

27 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

28 11/19/01UTexas Austin Seminar28 Phase center offsets  = dh cos  ; sin  = (R/a) sin  ; (R/a) = 0.24

29 11/19/01UTexas Austin Seminar29 Elevation angle dependence

30 11/19/01UTexas Austin Seminar30 Full estimation effects

31 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.

32 Total phase center position and adjustment to specified values

33 11/19/01UTexas Austin Seminar33 Scale variations with time

34 11/19/01UTexas Austin Seminar34 Center of mass variations as well

35 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

36 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)

37 11/19/01UTexas Austin Seminar37 Relativistic Effects

38 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)

39 11/19/01UTexas Austin Seminar39 Locations measured with GPS Red are campaign (~5000), other colors continuous GPS operated by different groups

40 11/19/01UTexas Austin Seminar40 Motion in North America Note rapid change in California Remainder of field consistent with rotating NA plate

41 11/19/01UTexas Austin Seminar41 Detail in Western United States

42 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

43 11/19/01UTexas Austin Seminar43 Motion in Turkey and Aegean

44 11/19/01UTexas Austin Seminar44 1999 Izmit Earthquake Black vectors are observed, Yellow model calculation

45 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

46 11/19/01UTexas Austin Seminar46 Other applications Aircraft positioning, vehicle navigation, engineering (real-time differential GPS links shown)

47 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

48 11/19/01UTexas Austin Seminar48 Clock effects GPS is controlled by 10.23 MHz oscillators On the Earth’s surface these oscillators are set to 10.23x(1-4.4647x10 -10 ) 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

49 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

50 11/19/01UTexas Austin Seminar50 Effects of Selective Availability

51 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


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