Mitigating Ionospheric Threat Using a Dense Monitoring Network

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Mitigating Ionospheric Threat Using a Dense Monitoring Network

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Concerns for MSAS The major concern for vertical guidance is ionosphere: The ionospheric term is dominant factor of protection levels; ... –

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Title: Mitigating Ionospheric Threat Using a Dense Monitoring Network


1
ION GNSS 2007 Fort Worth, TX Sept. 25-28, 2007
Mitigating Ionospheric Threat Using a Dense
Monitoring Network
T. Sakai, K. Matsunaga, K. Hoshinoo, K. Ito,
ENRI T. Walter, Stanford University
2
Introduction
  • The ionospheric effect is a major error source
    for SBAS
  • The ionospheric term is dominant factor of
    protection levels
  • Necessary to reduce GIVE values not only in the
    storm condition but also in the nominal condition
    to improve availability of vertical guidance.
  • The problem is caused by less density of IPP
    samples
  • The current planar fit algorithm needs inflation
    factor (Rirreg) and undersampled threat model to
    ensure overbounding residual error
  • Solution integrating the external network such
    as GEONET and CORS
  • Developed a GIVE algorithm suitable to such a
    situation.
  • Evaluated a new GIVE algorithm with GEONET
  • 100 availability of APV-II (VAL20m) at most of
    Japanese Airports
  • Still protects users No HMI condition found.

3
MSAS Status
  • All facilities installed
  • 2 GEOs MTSAT-1R (PRN 129) and MTSAT-2 (PRN 137)
    on orbit
  • 4 GMSs and 2 RMSs connected with 2 MCSs
  • IOC WAAS software with localization.
  • Successfully certified for aviation use
  • Broadcast test signal since summer 2005 with
    Message Type 0
  • Certification activities Fall 2006 to Spring
    2007.
  • Began IOC service on Sept. 27 JST (1500 Sept. 26
    UTC).

Launch of MTSAT-1R (Photo RSC)
4
Position Accuracy
_at_Takayama (940058) 05/11/14 to 16 PRN129
_at_Takayama (940058) 05/11/14 to 16 PRN129
GPS
GPS
MSAS
MSAS
Horizontal RMS 0.50m MAX 4.87m
Vertical RMS 0.73m MAX 3.70m
5
Concerns for MSAS
  • The current MSAS is built on the IOC WAAS
  • As the first satellite navigation system
    developed by Japan, the design tends to be
    conservative
  • The primary purpose is providing horizontal
    navigation means to aviation users Ionopsheric
    corrections may not be used
  • Achieves 100 availability of Enroute to NPA
    flight modes.
  • The major concern for vertical guidance is
    ionosphere
  • The ionospheric term is dominant factor of
    protection levels
  • Necessary to reduce GIVE to provide vertical
    guidance with reasonable availability.

6
APV-I Availability of IOC MSAS
MSAS Broadcast 06/10/17 0000-2400 PRN129
(MTSAT-1R) Test Signal Contour plot for APV-I
Availability HAL 40m VAL 50m Note
100 availability of Enroute through NPA
flight modes.
7
Components of VPL
VPL
Ionosphere (5.33 sUIRE)
Clock Orbit (5.33 sflt)
MSAS Broadcast 06/10/17 0000-1200 3011
Tokyo PRN129 (MTSAT-1R) Test Signal
  • The ionospheric term is dominant component of
    Vertical Protection Level.

8
Problem Less Density of IPP
  • Ionospheric component GIVE
  • Uncertainty of estimated vertical ionospheric
    delay
  • Broadcast as 4-bit GIVEI index.
  • Current algorithm Planar Fit
  • Vertical delay is estimated as parameters of
    planar ionosphere model
  • GIVE is computed based on the formal variance of
    the estimation.
  • The formal variance is inflated by
  • Rirreg Inflation factor based on chi-square
    statistics handling the worst case that the
    distribution of true residual errors is not
    well-sampled a function of the number of IPPs
    Rirreg 2.38 for 30 IPPs
  • Undersampled threat model Margin for threat that
    the significant structure of ionosphere is not
    captured by IPP samples a function of spatial
    distribution (weighted centroid) of available
    IPPs.

9
Using External Network
  • Integrating the external network to the SBAS
  • Increase the number of monitor stations and IPP
    observations dramatically at very low cost
  • Just for ionospheric correction Clock and orbit
    corrections are still generated by internal
    monitor stations because the current
    configuration is enough for these corrections
  • Input raw observations OR computed ionospheric
    delay and GIVE from the external network
    loosely-coupled systems.
  • Necessary modifications
  • A new algorithm to compute vertical ionospheric
    delay and/or GIVE is necessary because of a great
    number of observations
  • Safety switch to the current planar fit with
    internal monitor stations when the external
    network is not available.

10
Available Network GEONET
  • GEONET (GPS Earth Observation Network)
  • Operated by Geographical Survey Institute of
    Japan
  • Near 1200 stations all over Japan
  • 20-30 km separation on average.
  • Open to public
  • 30-second sampled archive is available as RINEX
    files.
  • Realtime connection
  • All stations have realtime datalink to GSI
  • Realtime raw data stream is available via some
    data providers.

GEONET station
MSAS station
11
Sample IPP Distribution
  • A snap shot of all IPPs observed at all GEONET
    stations at an epoch
  • GEONET offers a great density of IPP
    observations
  • There are some Japan-shape IPP clusters each
    cluster is corresponding to the associated
    satellite.

12
New Algorithms
  • (1) Residual Bounding
  • An algorithm to compute GIVE for given vertical
    delays at IGPs
  • Vertical delays are given For example, generated
    by planar fit
  • Determine GIVE based on observed residuals at
    IPPs located within 5 degrees from the IGP Not
    on the formal variance of estimation
  • Improves availability of the system.
  • (2) Residual Optimization
  • An algorithm to optimize vertical delays at IGPs
  • Here Optimum means the condition that sum
    square of residuals is minimized
  • GIVE values are generated by residual bounding
  • Improves accuracy of the system.

13
Residual Bounding (1)
  • An algorithm to compute GIVE for given vertical
    delays at IGPs
  • The MCS knows ionospheric correction function
    (bilinear interpolation) used in user receivers,
    Iv,broadcast(l,f), for given vertical delays at
    IGPs broadcast by the MCS itself
  • Residual error between the function and each
    observed delay at IPP, Iv,IPPi, can be computed
  • Determine GIVE based on the maximum of residuals
    at IPPs located within 5 degrees from the IGP.

Vertical delay for user
Observed delay at IPP
14
Residual Bounding (2)
  • Determine GIVE based on the maximum of residuals
    at IPPs located within 5 degrees from the IGP.

15
Residual Optimization
  • An algorithm to optimize vertical delays at IGPs
  • Vertical delays at IGPs can also be computed
    based on IPP observations as well as GIVE values
  • Again, define residual error between the user
    interpolation function and each observed delay at
    IPP, Iv,IPPi
  • The optimum set of vertical delays minimizes the
    sum square of residuals GIVE values are
    minimized simultaneously
  • The optimization can be achieved by minimizing
    the energy function (often called as cost
    function) following over IGP delays (See paper)

Function of IGP delays
16
Number of Available IPPs
  • The histogram of the number of IPPs available at
    each IGP (located within 5 deg from the IGP)
  • For 68 cases, 100 or more IPPs are available
  • Exceeds 1000 for 27 cases.

17
GIVE by Residual Bounding (1)
Planar Fit
Residual Bounding (All GEONET sites)
  • Histogram of computed GIVE values in typical
    ionospheric condition for two algorithms
  • Residual bounding with GEONET offers
    significantly reduced GIVE values
  • Blue lines indicate quantization steps for GIVEI.

18
GIVE by Residual Bounding (2)
Planar Fit
Residual Bounding (All GEONET sites)
  • Histogram of computed GIVE values in severe storm
    condition for two algorithms
  • The result is not so different from case of
    typical condition.

19
Reduction of GIVEI
Planar Fit
Residual Bounding (All GEONET sites)
  • Histogram of 4-bit GIVEI index broadcast to
    users
  • Lower limit of GIVEI is 10 for planar fit
  • Residual bounding can reduce GIVEI as well as
    GIVE values.

20
Comparison with FOC WAAS
Planar Fit (FOC WAAS)
Residual Bounding (All GEONET sites)
  • FOC WAAS Dynamic Rirreg, RCM, multi-state storm
    detector, and CNMP
  • GIVE values derived by residual bounding are
    still smaller than FOC WAAS algorithms.

21
Residual Optimization
  • Histogram of difference of IGP delays with and
    without residual optimization
  • Adjustment of IGP delay stays 0.052m
  • In comparison with quantization step of 0.125m,
    the effect is little.

22
User Position Accuracy
Planar Fit (RMS 1.47m)
Residual Bounding (RMS 1.10m)
Residual Optimization (RMS 1.10m)
  • User vertical position error at Tokyo in typical
    ionospheric condition
  • Residual bounding improves user position
    accuracy, while residual optimization is not
    effective so much.

23
Evaluation by Prototype SBAS
  • Prototype SBAS software developed by ENRI (NTM
    2006)
  • Computer software running on PC or UNIX
  • Generates the complete 250-bit SBAS messages
    every seconds
  • Simulates MSAS performance with user receiver
    simulator
  • Available as an MSAS testbed Measures benefit of
    additional monitor stations and evaluates new
    candidate algorithms.
  • Integration with the proposed algorithms
  • Scenario of vertical ionospheric delay and GIVE
    is generated based on GEONET archive data with
    application of the proposed algorithms
  • The prototype generated augmentation messages
    with ionospheric corrections induced as the
    scenario
  • Tested for typical ionospheric condition (July
    2004) and severe storm condition (October 2003).

24
User Protection
  • PPWAD Simulation
  • 03/10/29-31
  • 3011 Tokyo
  • Condition
  • Severe Storm
  • Algorithm
  • Residual Bounding
  • (All GEONET sites)
  • Users are still protected by this algorithm
    during the severe storm.

25
System Availability
PPWAD Simulation 04/7/22-24 Condition Typical
Ionosphere Algorithm Residual Bounding (All
GEONET sites) Contour plot for APV-II
Availability HAL 40m VAL 20m
26
Conclusion
  • Introduced new algorithms and usage of the
    external network to mitigate ionospheric threats
  • Algorithms for bounding ionospheric corrections
    based on optimization of residual error measured
    by dense monitoring network
  • Integration of GEONET as an external network.
  • Evaluation by prototype SBAS software
  • Reduced GIVEI enables 100 availability of APV-II
    flight mode (VAL20m) at most of Japanese
    airports
  • No integrity failure (HMI condition).
  • Further investigations
  • Consideration of threats against the proposed
    algorithms
  • Reduction of the number of stations required for
    residual bounding
  • Temporal variation and scintillation effects.

27
Announcement
  • Ionospheric delay database will be available
    shortly
  • The datasets used in this study and
  • Recent datasets generated daily from August 2007
  • Each dataset is a file which consists of slant
    delays observed at all available GEONET stations
    with 300-second interval Hardware biases of
    satellites and receivers are removed
  • Access to URL
  • http//www.enri.go.jp/sat/pro_eng.htm
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