Dual Frequency Measured Ionosphere correction May 3, 2000 |
Single Frequency Broadcast Ionosphere correction May 3, 2000 |
Single Frequency No Ionosphere correction May 3, 2000 |
| The images above demonstrate the effect
of ionospheric corrections on the accuracy of GPS data now that selective
availability (SA) is gone. Each plot shows the error in ellipsoidal height
of 24 hours of data (0000 to 2359 UTC) taken on May 03, 2000, by the Continuously
Operating Reference Stations (CORS) at Erlanger, Kentucky.
The image on the left displays height scatter after correcting for ionosphere
derived from L1 and L2 pseudoranges. The image in the center displays
height scatter after applying the GPS broadcast ionosphere model corrections
(ICD-GPS-200C) to the L1 pseudoranges. The image on the right displays
height scatter when no ionosphere correction is applied to the L1 pseudoranges.
The table at left summarizes the accuracies using different ionosphere corrections. Click on any of the results for a full-size image of the underlying 24-hour data set. The numbers in the table represent the +/- limit in meters bounding 95% of the computed heights. Now that SA has been removed, the impact of ionospheric and tropospheric error on height is clearly evident. As seen in the figures, the dual frequency correction does reduce the height error somewhat, but substantial systematic error in height is present in all cases. The patterns seen after the dual frequency correction are due to the troposphere error on the low elevation GPS satellites participating in the solution. In the interest of completeness, it should be pointed out that dual frequency ionosphere correction represents a measurement of the ionosphere, and is subject to the multipath error on both the L1 and L2 pseudoranges. The larger variation in the dual frequency results of May 5 and 19 are due to some disturbance (perhaps interference) in the L2 pseudoranges. For additional information: Dr. Richard SnayReturn to the GIAC REMOVAL OF GPS SELECTIVE AVAILABILITY page for more results. |
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| Fine Print: Data taken at the Erlanger National CORS station, National Geodetic Survey, at 30 second intervals. Instrumentation was an Ashtech Z-12 receiver. GPS data were both single-frequency (just L1) pseudorange and dual-frequency pseudorange (both L1 and L2). Data were processed in accordance with the GPS Interface Control Document ICD-GPS-200C, using the broadcast orbit parameters in the World Geodetic System WGS 84 (G873) reference system. The broadcast ionospheric model was only applied to specified single-frequency results. No troposphere models were applied. | ||