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GPS Milestones, cont. · 2020. 10. 1. · Orbit (Ephemeris) 2.5 0 Ionosphere 5.0 0.4 Troposphere...

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The Global Positioning Sytem, Part 1 10/1/2020 M. Helper, GEO 327G/386G, UT Austin 1 Geo327G/386G: GIS & GPS Applications in Earth Sciences Jackson School of Geosciences, University of Texas at Austin The Global Positioning System 10/1/2020 5-1 Geo327G/386G: GIS & GPS Applications in Earth Sciences Jackson School of Geosciences, University of Texas at Austin GPS Facts of Note US DoD navigation system First launch on 22 Feb 1978, fully operational in 1994 ~$15 billion (?) invested to date 24 (+/-) Earth-orbiting satellites (SVs) 24 primary, 7 spares; 32 presently in orbit Altitude of 20,200 km In 6 orbital planes inclined 55 o to equator, spaced 60 o apart Orbital period of 12 hrs 6 to 12 SVs visible at all times anywhere in the world EU Galileo, Russian Fed. GLONAS systems 10/1/2020 5-2 GPS Milestones 1978: First 4 satellites launched 1983: GPS declassified 1989: First hand-held receiver 1991: S/A activated DGPS now essential for surveying and mapping 1994: GPS constellation fully operational (My first hand-held receiver) 1995-1996: First hand-held, “mapping-grade” receivers (DGPS-enabled, w/data dictionary) (DGS gets 2, and buys 2 more 3 years later) 10/1/2020 3 GPS Milestones, cont. 1996-1998: GPS on a microchip (UT senior thesis student completes first geo. map with DGPS) 1997: First $100 hand-held receiver 1999: USCG DGPS service operational Free real-time DGPS for areas near waterways 2000: S/A off Detailed mapping with an inexpensive receiver now possible DGS buys 10 WAAS-enabled e-Trex receivers DGS begins teaching GIS/GPS course 2003: FAA commissions WAAS Free national DGPS coverage DGS/CNS purchases 35 more WAAS e-Trex DGS purchases 3 tablets with internal WAAS GPS and GeoXT 2008: DGS buys 10 mapping grade handhelds (Trim.Nomads) 10/1/2020 4
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  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 1

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    The Global Positioning System

    10/1/2020 5-1

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    GPS Facts of Note

    ❑US DoD navigation system❑First launch on 22 Feb 1978, fully operational in 1994

    ❑~$15 billion (?) invested to date

    ❑24 (+/-) Earth-orbiting satellites (SVs)❑24 primary, 7 spares; 32 presently in orbit

    ❑Altitude of 20,200 km❑In 6 orbital planes inclined 55o to equator, spaced 60o apart

    ❑Orbital period of 12 hrs

    ❑6 to 12 SVs visible at all times anywhere in the world

    ❑EU Galileo, Russian Fed. GLONAS systems

    10/1/2020 5-2

    GPS Milestones

    ◼ 1978: First 4 satellites launched

    ◼ 1983: GPS declassified

    ◼ 1989: First hand-held receiver

    ◼ 1991: S/A activated

    DGPS now essential for surveying and mapping

    ◼ 1994: GPS constellation fully operational• (My first hand-held receiver)

    ◼ 1995-1996: First hand-held, “mapping-grade” receivers (DGPS-enabled, w/data dictionary)

    • (DGS gets 2, and buys 2 more 3 years later)

    10/1/2020 3

    GPS Milestones, cont.

    ◼ 1996-1998: GPS on a microchip• (UT senior thesis student completes first geo. map with DGPS)

    ◼ 1997: First $100 hand-held receiver

    ◼ 1999: USCG DGPS service operational Free real-time DGPS for areas near waterways

    ◼ 2000: S/A off Detailed mapping with an inexpensive receiver now possible

    • DGS buys 10 WAAS-enabled e-Trex receivers

    • DGS begins teaching GIS/GPS course

    ◼ 2003: FAA commissions WAAS Free national DGPS coverage

    • DGS/CNS purchases 35 more WAAS e-Trex

    • DGS purchases 3 tablets with internal WAAS GPS and GeoXT

    • 2008: DGS buys 10 mapping grade handhelds (Trim.Nomads)

    10/1/2020 4

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 2

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    GPS Segments

    ❑Space – Satellites (SVs).

    ❑Control – Ground stations track SV orbits and monitor clocks, then update this info. (ephemeris, clock corrections) for each SV, to be broadcast to users (“almanac”). Control Facility at Schriever Air Force Base, CO.

    ❑User – GPS receivers convert SV signals into position, velocity and time estimates.

    10/1/2020 5-5

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Ranging Techniques

    ❑Two-way ranging: “Active”

    ❑Electronic Dist. Measuring devices (EDMs)

    ❑Radar, Sonar, Lidar

    ❑One-way ranging: “Passive”

    ❑GPS

    10/1/2020 5-6

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Ranging techniques

    ❑Two-way ranging (EDM)

    Light beam

    Range

    Range = C x DTime/2

    reflector

    10/1/2020 5-7

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Two-way Ranging: Electronic Distance Measuring (EDM) Instrument

    Retroreflector

    (“target” mirror)

    EDM:

    laser source/receiver

    10/1/2020 5-8

    Mt. Saint Helens Monitoring Prior to 1980 Eruption

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 3

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Ranging techniques

    ❑One-way ranging with GPS

    Range

    Radio Signal

    Range = C x DTime

    1 microsecond error = ~ 300 meters1 nanosecond error = ~ 1 foot

    “Sphere of position”

    10/1/2020 5-9

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    How are SV and receiver clocks synchronized?

    Clock errors will cause spheres of position (solid lines) to miss intersecting at a point.

    Adjust receiver clock slightly forward will cause larger DT(=larger sphere; dashed) and intersection at point.

    Requires 4 SVs, not 3 as shown, for clock error & X, Y, Z

    10/1/2020 5-10

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Satellite Positioning

    Geocenter

    Known

    Orbit

    Observe DT

    Determine

    10/1/2020 5-11

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    3-D (X, Y, Z) One-way Ranging

    ❑Intersection of 2 spheres of position yields circle

    ❑Intersection of 3 spheres of position yields 2 points of location

    ❑One point is position, other is either in space or within earth’s interior

    ❑With earth ellipsoid (4th sphere)❑Get receiver clock synchronized and X & Y

    but no Z

    ❑Intersection of 4 spheres of position yields XYZ and clock synchronization

    Two spheres

    Three spheres

    10/1/2020 5-12

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 4

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Determine Position by:

    1) Downloading almanac (ephemeris info., SV health, etc.) Takes 12.5 minutes for full message.

    2) Synchronize receiver clock/measure DT to 4 satellites = pseudorange

    3) Account for error sources (see below) by modeling = range

    4) Calculating intersection and compute X, Y, Z w.r.t. to center of selected reference ellipsoid

    5) Converting to coordinates of interest

    10/1/2020 5-13

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    How is DT measured?

    ❑By using broadcast signals (“codes”)

    ❑Code solutions

    ❑Less precise, easiest to achieve

    OR

    ❑By using carrier cycles

    ❑Carrier-phase solutions

    ❑More precise, more difficult to achieve

    10/1/2020 5-14

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Broadcast Signals - Codes

    ❑Each SV broadcasts unique C/A code❑1023 bits/millisecond, binary, pseudorandom

    ❑Receiver generates same codes

    ❖Precise or protected (P) code❑Authorized users only, more accurate (5-10 m absolute)

    ❑Code requires algorithm “seed” that is classified

    ❑P code for each satellite reset weekly

    ❖Y code❑Military use only

    ❑Code algorithm is encrypted

    ❖Status message – satellite health, status and orbit info

    +1

    -1

    ❖ Coarse acquisition (C/A) code• Civilian access, least accurate;

    10/1/2020 5-15

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Signal “Carrier”

    ❑Radio waves with following characteristics:

    ❑L1 (&L1c): frequency = ~1575 MHz with l = 19 cm❑Carries C/A code and status message, modulated at 1 MHz

    ❑Carries P code modulated at 10 MHz

    ❑L2 (&L2c ): frequency = ~1228 MHz with l = 24 cm❑Carries P code

    ❑Fundamental precision in positioning limited by ability to determine phase of carrier (to ~ 0.01l = 1 or 2 mm) l

    10/1/2020 5-16

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 5

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    DT Code solutions

    ❑Compare offsets in satellite and receiver codes to arrive at DT

    DT

    Pseudorange = C x DT

    +1

    -1

    Code generated by SV

    +1

    -1Code generated by receiver

    10/1/2020 5-17

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Sources of Error

    200 km

    50 km

    SV clock error (~1.5 m)+/- Selective Availability (~30 m)

    Ionospheric Refraction (~ 5 m)(Can correct with L1 & L2 DTs)

    Tropospheric Delay (~ 0.5 m)

    Multipathing (~0.5 m)

    + GDOP (errors x 2-12)(Geometric dilution of precision)

    L2

    L1

    Satellite Orbit Errors (~2.5 m)

    10/1/2020 5-18

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Range Uncertainties-DOPs

    From Bolstad, Fig. 5-11

    10/1/2020 5-19

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Geometric Dilution of Precision (GDOP)

    From Bolstad, Fig. 5-10

    10/1/2020 5-20

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 6

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Summary of Error Sources (m)Source: Trimble Navigation. Standard GPS DGPS

    SV Clocks 1.5 0

    Orbit (Ephemeris) 2.5 0

    Ionosphere 5.0 0.4

    Troposphere 0.5 0.2

    Receiver Noise 0.3 0.3

    Multipath 0.6 0.6

    S/A 30 (0) 0

    2-D Accuracy ~10-15m 2.8

    10/1/2020 5-21

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Solar Cycle – 2014 maximum

    10/1/2020 5-22

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Comparison with S/A on & off

    ❑S/A on: I’m in the stadium but am I on the field or in the stands?

    S/A off: Which yard marker am I on?

    10/1/2020 5-23

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Differential GPS (DGPS)

    ❑Requires two receivers

    ❑One receiver (base) is established at known position

    ❑Second receiver (rover) occupies unknown position(s)

    ❑Common errors are eliminated by combining data from both receivers

    ❑Most accurate results from use of carrier (L1, L2) phase DGPS (

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 7

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Differential GPS Positioning

    Base: known position Rover: unknown position

    Base station pseudoranges compared to known position; differences are errors common to both receivers.

    Base computes pseudorange corrections for rover.

    Apply correction to rover data, either in real time (+/-6 seconds) or long afterwards.

    10/1/2020 5-25

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Base Station Correction Data Availability:

    1. Real-time, via telemetry

    ❑Auxillary antenna connected to GPS receiver to receive broadcast corrections in real-time:

    ❑Ground-based augmentation Services (GBAS)❑Base station and broadcaster set up on site (JSG equipment)

    ❑US Coast Guard (US Nationwide Differential GPS System; NDGPS)

    ❑Satellite-based augmentation services (SBAS) ❑WAAS, EGNOS, Commercial Services – OmniSTAR

    2. After the fact, post-processing

    ❑Base station data combined with rover data after collection

    ❑CORS – continuously operating reference system (data from a network of base stations stored for download)

    10/1/2020 5-26

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Important Developments, DGPS

    ❑USCG DGPS beacon service (1999; NDGPS)

    ❑Deactivation of Selective Availability (S/A) (2000)

    ❑Satellite Based Augmentation Systems (SBAS)

    ❑Commissioning of US FAA Wide Area Augmentation System (WAAS) (2003)

    ❑European Union - EGNOS (2009)

    ❑OmniSTAR – Commercial service, global coverage

    10/1/2020 5-27

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    NDGPS Network – US Coast Guard

    April, 2015

    1-3 m accuracies!

    10/1/2020 5-28

    http://www.navcen.uscg.gov/dgps/coverage/GulfCoast.htmhttps://en.wikipedia.org/wiki/Wide_Area_Augmentation_Systemhttp://www.omnistar.com/howitworks.htmlhttp://www.ngs.noaa.gov/CORS/cors-data.html

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 8

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    2016 Decommissioning of NDGPS Sites?

    10/1/2020 5-29

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    NDGPS Beacon Service, Texas

    December, 2004

    10/1/2020 5-30

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    2003 Commissioning of WAAS

    ❑DGPS corrections broadcast from geostationary satellites

    10/1/2020 5-31

    Deactivation of Selective Availability

    Lati

    tud

    e (m

    )

    - 100 0 100Longitude (m)

    - 100

    100

    0

    Lati

    tud

    e (m

    )

    - 100 0 100Longitude (m)

    - 100

    100

    0

    S/A On, 5-1-2000 S/A Off, 5-3-2000

    ~25 m

    ~100 m

    10/1/2020 33

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 9

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Signal “Carrier”

    ❑Radio waves with following characteristics:

    ❑L1: frequency = ~1575 MHz with l = 19 cm❑Carries C/A code and status message, modulated at 1 MHz

    ❑Carries P code modulated at 10 MHz

    ❑L2: frequency = ~1228 MHz with l = 24 cm❑Carries P code

    ❑Fundamental precision in positioning limited by ability to determine phase of carrier (to ~ 0.01l = 1 or 2 mm) l

    10/1/2020 5-34

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    DGPS Carrier-Phase Solutions

    Use 19 cm wave as ruler to measure # of cycles (& phase of cycle) from each satellite

    Ruler is not labeled; track phase from several SVs and find intersection(s) of coincident phases.

    Know approx. position of antenna from code-phase DGPS; eliminates ambiguity.

    Passage of waves and motion of SVs need to be known

    Cycle Slips Sub-centimeter precision possible

    10/1/2020 5-35

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Types of Carrier-phase Solutions

    ❑Static: “Rover” is stationary and collects data for several hours

    ❑Rapid Static: Rover is stationary and collects for 5-20 minutes

    ❑Kinematic: Rover collects on the move

    10/1/2020 5-36

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    Accuracy of Code vs. Carrier Phase Solutions

    Code Solutions

    Carrier Phase

    Solutions

    10/1/2020 5-37

  • The Global Positioning Sytem, Part 1 10/1/2020

    M. Helper, GEO 327G/386G, UT Austin 10

    Geo327G/386G: GIS & GPS Applications in Earth SciencesJackson School of Geosciences, University of Texas at Austin

    GPS Accuracy – Generic Terminology

    Satellite-Based Augmentation Systems, e.g. WAAS, EGNOS

    Differential Global Navigation

    Satellite System, e.g. NDGPS

    of US Coast Guard

    Ground Based Augmentation Systems (aviation), e.g. LAAS

    Wide-Area Real-Time Kinematics

    (not yet realized)Precise Point Positioning

    Autonomous (single receiver)

    Real-Time Kinematics

    10/1/2020 5-38

    R.F

    . map

    sca

    le

    Horizontal Resolution, meters

    3 6 12 25 100

    GPS Precision and Map Scales

    50 - 20 K S/A off (2000)10 – 25 m

    15 - 4 KDGPSWAAS (2003)

    1.5 – 3 m

    6 - 2 K DGPS beacon(e.g. USCG)

    1 – 3 m

    1:200 K S/A on (1991)100 m


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