T. Sakai, K. Matsunaga, K. Hoshinoo, ENRIT. Walter, Stanford .ppt
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1、T. Sakai, K. Matsunaga, K. Hoshinoo, ENRI T. Walter, Stanford University,Modeling Ionospheric Spatial Threat Based on Dense Observation Datasets for MSAS,ION GNSS 2008 Savannah, GA Sept. 16-19, 2008,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 1,The ionospheric effect is a major error source for SBAS: The
2、 ionospheric term is the dominant factor of protection levels; Necessary to develop ionosphere algorithms reducing ionospheric component of protection levels to improve availability of vertical guidance. Threat model should be prepared for new algorithms: Any algorithms need the associate spatial th
3、reat model to ensure overbounding residual error; The threat model depends upon the algorithms; Developed a methodology to create a spatial threat model. Threat models created by the proposed methodology: Evaluation of the current MSAS threat model; Some new threat models evaluated; System availabil
4、ity also evaluated.,Introduction,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 2,MSAS Status,Launch of MTSAT-1R (Photo: RSC),All facilities installed: 2 GEOs: MTSAT-1R (PRN 129) and MTSAT-2 (PRN 137) on orbit; 4 domestic GMSs and 2 RMSs (Hawaii and Australia) connected with 2 MCSs; IOC WAAS software with l
5、ocalization. Successfully certified for aviation use. IOC service since Sept. 27, 2007; Certified for Enroute to NPA operations; Approved for navigation use in Japanese FIR.,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 3,Position Accuracy,Horizontal RMS 0.50m MAX 4.87m,Vertical RMS 0.73m MAX 3.70m,GPS,MSA
6、S,GPS,MSAS,Takayama (940058) 05/11/14 to 16 PRN129,Takayama (940058) 05/11/14 to 16 PRN129,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 4,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 prov
7、iding horizontal navigation means to aviation users; Ionopsheric corrections may not be used; Achieves 100% availability of Enroute to NPA flight modes.,Concerns for MSAS,The major concern for vertical guidance is ionosphere: The ionospheric term is dominant factor of protection levels; Necessary to
8、 reduce ionospheric term to provide vertical guidance with reasonable availability.,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 5,NPA Availability,100% Everywhere,MSAS Broadcast 08/1/17 00:00-24:00PRN129 (MTSAT-1R) Operational SignalContour plot for: NPA AvailabilityHAL = 556mVAL = N/A,100% Availability
9、for Enroute thru NPA.,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 6,APV-I Availability,MSAS Broadcast 08/1/17 00:00-24:00PRN129 (MTSAT-1R) Operational SignalContour plot for: APV-I AvailabilityHAL = 40mVAL = 50m,Vertical guidance cannot be provided by the current MSAS.,ION GNSS 16-19 Sept. 2008 - ENRI,SL
10、IDE 7,Components of VPL,The ionospheric term (GIVE) is dominant component of Vertical Protection Level.,VPL,Clock & Orbit (5.33 sflt),Ionosphere (5.33 sUIRE),MSAS Broadcast 06/10/17 00:00-12:00 3011 TokyoPRN129 (MTSAT-1R) Test Signal,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 8,Ionosphere Term: GIVE,Ion
11、ospheric 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
12、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
13、ionosphere is not captured by IPP samples; a function of spatial distribution (weighted centroid) of available IPPs.,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 9,Planar Fit and GIVE,Developed for WAAS; MSAS employs the same algorithm;Assume ionospheric vertical delay can be modeled as a plane;Model para
14、meters are estimated by the least square fit;GIVE (grid ionosphere vertical error): Uncertainty of the estimation including spatial and temporal threats.,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 10,Ionospheric Spatial Threat,Planar fit is performed with IPPs (ionospheric pierce points) measured by GMS
15、 stations; Local irregularities might not be sampled by any GMS stations;Users might use IPPs within the local irregularities; Potential threat of large position error;MSAS must protect users against such a condition; The spatial threat term is added to GIVE;Spatial threat model created based on the
16、 historical severe ionospheric storm data.,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 11,Example of Spatial Threat Model,Max Residual,Threat Model,Function of fit radius (cutoff radius) and RCM metric; Good and bad IPP geometries are distinguished by these two metrics; Resulted sundersampled is roughly
17、between 0 and 2.5.,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 12,The Second Metric: RCM,RCM (Relative Centroid Metric) is used as the second metric of the threat model; The first one is fit radius;RCM is the distance between the weighted centroid of IPPs and IGP divided by fit radius;Using Rfit and RCM,
18、 it is possible to distinguish good and bad geometries of IPP distribution, and thus reduce undersampled threat term;For detail, see Ref. 11.,Weighted centroid of IPPs,ION GNSS 16-19 Sept. 2008 - ENRI,SLIDE 13,Methodology: Data Deprivation,Removes some IPPs (shown in red) for planar fit; They become
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