# Global Positioning System: what it is and how we use it for measuring the earth’s movement. April 21, 2011.

## Presentation on theme: "Global Positioning System: what it is and how we use it for measuring the earth’s movement. April 21, 2011."— Presentation transcript:

Global Positioning System: what it is and how we use it for measuring the earth’s movement.
April 21, 2011

References Lectures from K. Larson’s “Introduction to GNSS” Strang, G. and K. Borre “Linear Algebra, Geodesy, and GPS”, Wellesley-Cambridge Press, 1997 Blewitt, G., “Basics of the GPS Technique: Observation Equations”, in “Geodetic Applications of GPS” Lecture notes from G. Mattioli’ (comp.uark.edu/~mattioli/geol_4733/GPS_signals.ppt)

Basics of how it works Trilateration GPS positioning requires
distance to 4 satellites x,y,z,t Earth centered, Earth Fixed Why t? What are some of reasons why measuring distance is difficult? How do we know x, y, z, t of satellites?

GPS: Space segment Several different types of GPS satellites (Block I, II, II A, IIR) All have atomic clocks Stability of at least sec 1 sec every ~300,000 yrs Dynamics of orbit? Reference point?

Orbital Perturbations – (central force is 0.5 m/s2)
Source Acceleration m/s2 Perturbation 3 hrs Type Earth oblateness (J2 ) 5 x 10-5 2 3 hrs secular + 6 hr Sun & moon 5 x 10-6 hrs secular + 12hr Higher Harmonics 3 x 10-7 hrs Various Solar radiation pressure 1 x 10-7 days Secular + 3 hr Ocean & earth tides 1 x 10-9 days Earth albedo pressure days From K. Larson

GPS: Space Segment 24+ satellites in orbit
Can see 4 at any time, any point on earth Satellites never directly over the poles For most mid-latitude locations, satellites track mainly north-south

GPS: Satellite Ground Track

GPS Signal Satellite transmits on two carrier frequencies:
L1 (wavelength=19 cm) L2 (wavelength=24.4 cm) Transmits 3 different codes/signals P (precise) code Chip length=29.3 m C/A (course acquisition) code Chip length=293 m Navigation message Broadcast ephemeris (satellite orbital parameters), SV clock corrections, iono info, SV health Say something about PRN numbers?

GPS Signal Signal phase modulated: vs
Amplitude modulation (AM) Frequency modulation (FM)

C/A and P code: PRN Codes
PRN = Pseudo Random Noise Codes have random noise characteristics but are precisely defined. A sequence of zeros and ones, each zero or one referred to as a “chip”. Called a chip because they carry no data. Selected from a set of Gold Codes. Gold codes use 2 generator polynomials. Three types are used by GPS C/A, P and Y

PRN Codes: first 100 bits

PRN Code properties High Autocorrelation value only at a phase shift of zero. Minimal Cross Correlation to other PRN codes, noise and interferers. Allows all satellites to transmit at the same frequency. PRN Codes carry the navigation message and are used for acquisition, tracking and ranging.

PRN Code Correlation

Non-PRN Code Correlation

Schematic of C/A-code acquisition
Since C/A-code is 1023 chips long and repeats every 1/1000 s, it is inherently ambiguous by 1 msec or ~300 km.

BASIC GPS MEASUREMENT: PSEUDORANGE
Receiver measures difference between time of transmission and time of reception based on correlation of received signal with a local replica The measured pseudorange is not the true range between the satellite and receiver. That is what we clarify with the observable equation.

PSEUDORANGE OBSERVABLE MODEL

CARRIER PHASE MODEL

COMPARE PSEUDORANGE and CARRIER PHASE
bias term N does not appear in pseudorange ionospheric delay is equal magnitude but opposite sign troposphere, geometric range, clock, and troposphere errors are the same in both multipath errors are different (phase multipath error much smaller than pseudorange) noise terms are different (factor of 100 smaller in phase data)

Atmospheric Effects Ionosphere (50-1000 km)
Delay is proportional to number of electrons Troposphere (~16 km at equator, where thickest) Delay is proportional to temp, pressure, humidity.

Vertical Structure of Atmosphere

Tropospheric effects Lowest region of the atmosphere – index of refraction = ~ at sea level Neutral gases and water vapor – causes a delay which is not a function of frequency for GPS signal Dry component contributes 90-97% Wet component contributes 3-10% Total is about 2.5 m for zenith to 25 m for 5 deg

Tropospheric effects At lower elevation angles, the GPS signal travels through more troposphere.

Dry Troposphere Delay Saastamoinen model:
P0 is the surface pressure (millibars) f is the latitude h is the receiver height (m) Hopfield model: hd is 43km T0 is temperature (K) Mapping function: E – satellite elevation ~2.5 m at sea level 1 (zenith) – 10 (5 deg)

Wet Troposphere Correction
Less predictable than dry part, modeled by: Saastamoinen model: Hopfield model: hw is 12km e0 is partial pressure of water vapor in mbar Mapping function: 0 – 80 cm

Examples of Wet Zenith Delay

Ionosphere effects • Pseudorange is longer – “group delay”
• Carrier Phase is shorter – “phase advance” TEC = Total Electron Content

Determining Ionospheric Delay
Where frequencies are expressed in GHz, pseudoranges are in meters, and TEC is in TECU’s (1016 electrons/m2)

Ionosphere maps

Ionosphere-free Pseudorange
Ionosphere-free pseudoranges are more noisy than individual pseudoranges.

Multipath Reflected signals Can be mitigated by antenna design
Multipath signal repeats with satellite orbits and so can be removed by “sidereal filtering”

Standard Positioning Error Budget
Single Frequency Double Frequency Ephemeris Data 2 m Satellite Clock Ionosphere 4 m 0.5 – 1 m Troposphere Multipath 0-2 m UERE 5 m 2-4 m UERE = User Equivalent Range Error

Intentional Errors in GPS
S/A: Selective availability Errors in the satellite orbit or clock Turned off May 2, 2000 With SA – 95% of points within 45 m radius. SA off, 95% of points within 6.3 m • Didn’t effect the precise measurements used for tectonics that much. Why not?

Intentional Errors in GPS
A/S: Anti-spoofing Encryption of the P code (Y code) Different techniques for dealing with A/S Recover L1, L2 phase Can recover pseudorange (range estimated using P-code) Generally worsens signal to noise ratio

AS Technologies Summary Table
Ashtech Z-12 & µZ Trimble 4000SSi From Ashjaee & Lorenz, 1992

PSEUDORANGE OBSERVABLE MODEL

EXAMPLE OF PSEUDORANGE (1)

EXAMPLE OF PSEUDORANGE (2)

GEOMETRIC RANGE Distance between position of satellite at time of transmission and position of receiver at time of reception

PSEUDORANGE minus GEOMETRIC RANGE
Difference is typically dominated by receiver clock or satellite clock.

L1 PSEUDORANGE - L2 PSEUDORANGE
Differencing pseudoranges on two frequencies removes geometrical effects, clocks, troposphere, and some ionosphere

Geometry Effects: Dilution of Precision (DOP)

Dilution of Precision Covariance is purely a function of satellite geometry

Dilution of Precision

Dilution of Precision (VDOP)
Casey station, Antarctica, 66.3 latitude Wuhan, China, 30 lat

Positioning • Most basic: solve system of range equations for 4 unknowns, receiver x,y,z,t P1 = ( (x1 - x)2 + (y1 - y)2 + (z1 - z)2 )1/2 + ct - ct1 P4 = ( (x4 - x)2 + (y4 - y)2 + (z4 - z)2 )1/2 + ct - ct4 Linearize problem by using a reference, or a priori, position for the receiver Even in advanced software, need a good a priori position to get solution.

Positioning vs. Differential GPS
By differencing observations at two stations to get relative distance, many common errors sources drop out. The closer the stations, the better this works Brings precision up to mm, instead of m.

Single Differencing • Removes satellite clock errors
• Reduces troposphere and ionosphere delays to differential between two sites • Gives you relative distance between sites, not absolute position

Double Differencing • Receiver clock error is gone
• Random errors are increased (e.g., multipath, measurement noise) • Double difference phase ambiguity is an integer

High precision GPS for Geodesy
Use precise orbit products (e.g., IGS or JPL) Use specialized modeling software GAMIT/GLOBK GIPSY-OASIS BERNESE These software packages will Estimate integer ambiguities Reduces rms of East component significantly Model physical processes that effect precise positioning, such as those discussed so far plus Solid Earth Tides Polar Motion, Length of Day Ocean loading Relativistic effects Antenna phase center variations

High precision GPS for Geodesy
Produce daily station positions with 2-3 mm horizontal repeatability, 10 mm vertical. Can improve these stats by removing common mode error.

Download ppt "Global Positioning System: what it is and how we use it for measuring the earth’s movement. April 21, 2011."

Similar presentations