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Altimeter crossovers from MOLA were used to evaluate the geopotential
solutions MGM0890I, MGM0964C5A, MGM0964C18, and the MGM0964C20.
The altimeter crossovers have the advantage of being completely
independent data, and are globally distributed.
Altimeter crossovers were formed for four five to six day arcs from
starting on March 7, March 13, March 18, and March 23, 1999.
Between 940 to 980 crossovers were computed
internally to each arc. No crossovers were formed if telemetered
spacecraft quaternions were missing for either the descending or ascending
track of a potential crossover point.
The modelling of the altimeter crossovers is described in Rowlands
et al.[28].
Altimeter crossovers from the highly eccentric orbits in SPO
were used to estimate corrections to the preflight measurements of
the orientation of the MOLA instrument with respect to the spacecraft
frame[6,28]. These new offset values of
-0.0028
in roll,and -0.0086
in pitch were simply applied in
the current tests with the mapping orbit altimetry.
The crossovers are not used in these orbit determination solutions, which
were determined solely from the range and the Doppler data for each
gravity field model. The crossovers are editted for off nadir pointing angles,
as well as the slope and the roughness of the terrain. Large crossover residuals
(greater than 80 m) were eliminated.
Because of the edit criterion of 80 m, the number of crossovers is
not identical in all of the test arcs.
The results are tabulated in Table 7 in aggregate for all four arcs.
The crossovers show the same trend as the orbit overlaps, and the
fits to the Doppler data. The crossover RMS is reduced as the fields are
refined, and show the best performance with the MGM0964C20 field.
| Table 7: MGS orbit performance measured by altimeter crossovers |
| Model |
Doppler |
Crossovers |
| |
No. of obs. |
RMS (mm/s) |
No. of obs. |
RMS (m) |
| MGM0890I |
14,838 |
18.93 |
3400 |
21.04 |
| MGM0964C5A |
14,838 |
1.65 |
3455 |
5.61 |
| MGM0964C18 |
14,838 |
0.84 |
3449 |
5.57 |
| MGM0965C20 |
14,838 |
0.53 |
3455 |
5.01 |
It is of interest to see whether the crossovers can still contribute
to orbit improvement in the near-circular orbit. Crossovers were processed
simultaneously with the Doppler tracking in four arcs of March 1999.
Empirical once per revolution along-track accelerations
were adjusted daily for these arcs, in addition to a drag coefficient
per day, a reflectivity coefficient per arc, and the empirical accelerations
for the AMD events.
March 1999 is a particularly tough test for the
crossovers since the Doppler data - although sparse, are of high quality.
In addition, the Doppler data in March 1999 were used
in the MGM0964C20 solution. The average RMS overlap
is shown in Table 8 for the three overlaps of these arcs.
| Table 8: MGS Orbit Overlaps with Altimeter Crossovers |
| Model |
Orbit Overlap Differences
(m)1 |
| |
Radial |
Cross-track |
Along-track |
Total |
| No Crossovers |
0.59 |
0.81 |
1.83 |
2.17 |
| With Crossovers |
0.26 |
1.40 |
0.90 |
1.73 |
1 Average RMS of three overlaps for four arcs from March 6, to March 23, 1999
The addition of the crossover data improves the orbits overall, and
especially in the radial, and the along-track directions. Some degradation
is observed in the cross-track direction.
It is especially encouraging that the consistency in the radial direction
has been further improved from 0.59 to 0.26 meters. The use of these
additional data in the form of altimeter crossovers allows
extra empirical parameters to be adjusted - for instance cross-track
once per revolution empirical accelerations - that would further
improve these orbit consistency results.
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Up: GRAVITY FIELD IMPROVEMENT
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Shelley Rowton
1999-10-20