24 Hour SA-Free Data – Ionosphere effects on Ellipsoidal Height

[graph]
Dual Frequency
Measured Ionosphere correction
May 3, 2000
[graph]
Single Frequency
Broadcast Ionosphere correction
May 3, 2000
[graph]
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.
 
Date Dual Freq.

Measured
Ionosphere
correction
95%

Single Freq.

Broadcast
Ionosphere
correction
95%

Single Freq.

No
Ionosphere
correction
95%

May 03 19.88 m 19.33 m 32.27 m
May 04 21.02 m 19.89 m 29.45 m
May 05 27.91 m * 21.94 m 32.08 m
May 06 20.73 m 21.69 m 31.32 m
May 07 20.59 m 22.45 m 31.43 m
May 08 21.25 m 24.20 m 32.17 m
May 09 19.89 m 21.96 m 31.88 m
May 10 20.50 m 22.86 m 31.08 m
May 11 20.78 m 21.07 m 31.54 m
May 12 21.36 m 19.04 m 30.33 m
May 13 -- data set incomplete --
May 14 19.46 m 17.68 m 29.83 m
May 15 20.36 m 19.56 m 32.81 m
May 16 20.71 m 20.34 m 33.83 m
May 17 19.50 m 20.99 m 29.49 m
May 18 21.02 m 20.11 m 32.95 m
May 19 23.35 m * 21.33 m 31.62 m
May 20 20.95 m 20.66 m 32.74 m
May 21 19.84 m 19.81 m 32.08 m
May 22 21.33 m 21.09 m 32.37 m
May 23 21.11 m 20.93 m 33.58 m
May 24 22.84 m 21.20 m 32.08 m
May 25 21.36 m 19.29 m 29.82 m
May 26 21.28 m 17.81 m 29.25 m
May 27 21.36 m 20.83 m 32.13 m
May 28 21.01 m 21.69 m 30.88 m
May 29 20.82 m 21.27 m 29.39 m
May 30 20.92 m 20.48 m 29.46 m
May 31 22.40 m 21.77 m 30.13 m
* Note: May 5 & May 19 data sets have L2 disturbance.

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 Snay
National Geodetic Survey, NOAA
Richard Snay
Return to the GIAC REMOVAL OF GPS SELECTIVE AVAILABILITY page for more results.
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.