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02/11/2003 12.080 GPS 1
Applications of the GlobalPositioning System
Prof. Thomas HerringDepartment of Earth, Atmosphere
and Planetary Sciences12.080 Seminar Spring 2003.http://www-gpsg.mit.edu/~tah
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Overview
• Original design of the Global PositioningSystem (GPS)
• Use by “non-authorized” users• Applications to:
– Tectonic studies– Meteorology– Other applications
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GPS Original Design• Started development in the late 1960s
as NAVY/USAF project to replaceDoppler positioning system
• Aim: Real-time positioning to < 10meters, capable of being used on fastmoving vehicles.
• Limit civilian (“non-authorized”) users to100 meter positioning.
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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-randomsequence (designated by PRN, PR number):Spread-spectrum transmission.
– Dual frequency band transmission:• L1 ~1.5 GHz, L2 ~1.25 GHz
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Latest Block IIR satellite(1,100 kg)
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Measurements• Measurements:
– Time difference between signal transmission fromsatellite and its arrival at ground station (called“pseudo-range”, precise to 0.1–10 m)
– Carrier phase difference between transmitter andreceiver (precise to a few millimeters)
– Doppler shift of received signal• All measurements relative to “clocks” in
ground receiver and satellites (potentiallyposes problems).
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Measurement usage• “Spread-spectrum” transmission:
Multiple satellites can be measured atsame time.
• Since measurements can be made atsame time, ground receiver clock errorcan be determined (along with position).
• Signal
V(t, r x ) = Vo sin[2p( ft -r k .r x ) + pC(t)]
C(t) is code of zeros and ones (binary).Varies discretely at 1 or 10 MHz
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Measurements• Since the C(t) code changes the sign of the
signal, satellite can be only be detected if thecode is known (PRN code)
• Multiple satellites can be separated by“correlating” with different codes (only thecorrect code will produce a signal)
• The time delay of the code is the pseudo-range measurement.
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PositionDetermination
(perfectclocks).
• Three satellitesare needed for 3-D position withperfect clocks. • Two satellitesare OK if height isknown)
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Positiondetermination:
with clockerrors: 2-D
case• Receiver clock isfast in this case, soall pseudo-rangesare short
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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 bysatellite in “broadcast ephemeris”
• “Differential” positioning (DGPS)eliminates need for accurate satelliteclock knowledge.
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Satellite constellation
• Since multiple satellites need to be seenat 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)
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Current constellation• Relative sizescorrect (inertialspace view)• “Fuzzy” linesnot due to orbitperturbations,but due tosatellites beingin 6-planes at55o inclination.
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Ground TrackPaths followed by satellite along surface of Earth.
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Satellite AvailabilitySatellite Availability (smallest number above
15o minimum elevation)
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Pseudo-range accuracy• Original intent was to position using pseudo-
range: Accuracy better than planned• C/A code (open to all users) 10 cm-10 meters• P(Y) code (restricted access since 1992) 5
cm-5 meters• Value depends on quality of receiver
electronics and antenna environment.
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GPS Antennas (for precise positioning)
• Rings arecalled choke-rings (used tosuppressmulti-path)
Nearly all antennas are patch antennas (conductingpatch mounted in insulating ceramic).
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Positioning accuracy• Best position accuracy with pseudo-
range is about 20 cm (differential) andabout 5 meters point positioning.
• For Earth science applications we wantbetter accuracy
• For this we use “carrier phase” where“range” measurement noise is fewmillimeters
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Carrier phase positioning• To use carrier phase, need to make
differential measurements between groundreceivers.
• Simultaneous measurements allow phaseerrors in clocks to be removed i.e. the clockphase error is the same for two groundreceivers observing a satellite at the sametime (interferometric measurement).
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Phase positioning
• Use of carrier phase measurementsallows positioning with millimeter levelaccuracy and sub-millimeter ifmeasurements are averaged for 24-hours.
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Examples ofpositioning
results
-0.10
-0.05
0
0.05
0.10
8 10 12 14 16 18 20 22 24
North
(m)
Time (hrs)
Phase Differential Positioning
Scatter 0.008 m and 0.002 m
-200
-100
0
100
200
8 10 12 14 16 18 20 22 24
North
(m)
Time (hrs)
Pseudorange Point Positioning
Scatter 21 m and 23 m
-2.0
-1.0
0.0
1.0
2.0
8 10 12 14 16 18 20 22 24
North
(m)
Time (hrs)
Pseudorange Differential Positioning
Scatter 0.20 m and 0.15 m
SAon
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Summary
• Use of differential measurements withcarrier phase allows very preciseposition determination (independentlargely of security features).
• We use these measurements in Earthscience for deformation studies andatmospheric studies
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Schematic of signal propagation• GPS signals retardedby propagation throughatmosphere• Ionosphere (plasma)is accounted by linearcombination ofmeasurements at L1and L2 frequencies.
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Atmospheric delays• Delay of signal due to atmosphere refraction
is 2.3-30 meters, depending on elevationangle
• Elevation angle dependence can be used toestimate amount of delay due to atmosphere
• For GPS frequencies, this delay dependsgreatly on the amount of water vapor inatmosphere
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GPS Measurements of precipitable water vapor (real-time)
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Tectonic Deformation Results• “Fixed GPS” stations operate continuously
and by determining their positions each daywe can monitor their motions relative to aglobal coordinate system
• Temporary GPS sites can be deployed onwell defined marks in the Earth and themotions of these sites can be monitored(campaign GPS)
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Locations measured with GPS
• Red are campaign (~5000), other colors continuousGPS operated by different groups
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Example of motions measured in Pacific/Asia region
• Fastest motionsare >100 mm/yr• Noteconvergencenear Japan
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Motion in North America
• Note rapidchange inCalifornia• Remainderof fieldconsistentwith rotatingNA plate
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Detail in Western United States
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CaliforniaDetail
• Compilation ofcontinuous andcampaign GPS• Only s<1.5 mm/yrshown• In 100 years, fastestpoints move 5 m
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Detailed view of LA Basin
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Motion in Turkey and Aegean
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1999 Izmit EarthquakeBlack vectors are observed, Yellow model calculation
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Motion after Earthquakes. Example fromHector Mine, CA
Continued motion tells us about material characteristicsand how stress is re-distributed after earthquake
-40
-30
-20
-10
0
10
20
30
1999.0 1999.5 2000.0 2000.5 2001.0 2001.5 2002.0 2002.5 2003.0
Pre-Hector MinePost_Hector mine
Diffe
renc
e fro
m M
ean
(mm
)
Year
Time of Hector mine earthquake220 mm offset removed
RMS Scatter about linear trend 0.8 mm
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Atmospheric pressure loading
-20
-10
0
10
20
1999.95 2000.00 2000.05 2000.10 2000.15
JPLMITAtm Load
DRAO
Hei
ght (
mm
)
Year
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Relativistic Effects
-50
-25
0
25
50
0 4 8 12 16 20 24
PRN 03 Detrended; e=0.02Clock - trend (ns)GR Effect (ns)
Cloc
k er
ror (
ns)
Time (hrs)
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Other applications• Aircraft positioning, vehicle navigation, engineering(real-time differential GPS links shown)
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Conclusions
• GPS dual-use technology: Applicationsin 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)• System modifications to support civilian
users better underway