Analysis of tracking experiments performed in February 1998
Analysis of tracking experiments performed in February 1998
Summary
On 25 Feb 1998 tracking experiments were performed in order
to derive an `efficiency' measure for the track model following
the Azimuth Track Upgrades program. Comparison with similar experiments
done in
1995 , and quantification of any improvement, is problematic,
although deviations from unity are likely to be less than 5%.
The data are in some aspects quite repeatable and suggest a change in the
multiplicative yaw factor, from 0.83 to
1.21, which I hope to test on
980410 . However, many 5" pointing
glitches appear in the data, are not necessarily associated
with
joints , and remain unexplained and seemingly unpredictable.
The datasets
As in 1995 (see the report
MTPPN05 - specifically the Section titled
`No-track pointing and tracking' ), tracking was done with the track
model disabled, and a
comparison made of observed and predicted pointing errors.
SCUBA was not available so RxA2 tuned to its mid-range was used.
Bright sources were essential to enable rapid pointing determinations
and hence good azimuth resolution. In the absence of planets at this time,
the quasars 3c273, 3c279 were used. 3c273 was followed over a large
azimuth range that includes 16
wheel/joint interactions , and 3c279 was followed over the last 4 of
these.
Source HST azimuth elevation
3c273 01:18 - 04:01 133 - 234 65 - 61
3c279 04:06 - 05:05 215 - 234 59 - 49
The seeing was erratic early on but stabilized for the latter
part of the experiment :
HST 01:00 02:00 02:30 04:00 05:00 HST
seeing 1.0 1.7 0.5 0.4 0.3 "
Pointing errors are
predicted from the track model, and
plots of the observed and predicted errors, their
differences and ratios can be seen by selecting the entries in the
table below :
The azimuths of the track joints are shown by the green vertical lines.
The observed azimuth errors in the azimuth range
215 to 234 are very repeatable (read `systematic'). For instance, for both
the 3c273 data
and the 3c279 data, plots of (daz_obs - daz_pre) -vs- azimuth
(the green traces in the above plots) show a
positive `hump' at about azimuth 220, followed by a negative spike
at azimuth 223. The larger 3c273 dataset also shows difference
spikes of amplitude ~5", particularly at azimuths 142 and 174, that are
associated with
wheel/joint interactions .
In contrast, the behaviour in elevation errors
appear to be quite random, except perhaps for a 2" or 3" glitch
at azimuth 155, which is unassociated with a
joint .
One measure of the goodness of fit of the track model is the scatter
in the difference plots (the green lines) :
Source az range N ------------- rms scatter --------------
(daz_obs - daz_pre) (del_obs - del_pre)
3c273 133 - 234 73 1.8 1.2
3c273 215 - 234 20 1.3 0.9
3c279 215 - 234 27 1.3 0.6
The large-ish value of 1.8 seems to be due in part to the curvature of the
(green) (daz_obs - daz_pre) -vs- azimuth line rather than to
(particularly) poor behaviour at the joints.
Straight line fits were made to the plots of Observed-Errors -vs-
Predicted-Errors for each of daz and del, and are shown in the
plots accessible from the above table. The straight line fits are of
the form
O_daz = m_daz * P_daz + const_daz
O_del = m_del * P_del + const_del
and the following results were obtained :
Source azimuths N m_daz +- rms m_del +- rms
3c273 133 - 234 73 1.22 0.05 1.6 0.99 0.04 1.2
3c273 215 - 234 20 1.01 0.12 1.4 0.94 0.06 0.9
3c279 215 - 234 27 1.06 0.10 1.3 0.98 0.04 0.6
Note that the rms's of the observed data about these lines are still
sufficiently larger than the expected accuracy of the predictions
(0.35 arcseconds) that the predicted data may be regarded as the
independent variable in this relationship.
The derived values of m_daz and m_del are, in their general range, not
unlike those seen in
1995 . The efficiency of the track model in representing the
motion of the telescope is again essentially 100%, with uncertainties
between 5% and 20%. In the shorter (20 degree) azimuth ranges covered
twice in these experiments, the efficiency, in both coordinates, is
typically 5%. Only the azimuth performance over the 100 degrees or so of
the 3c273 data implies an efficiency unlike 100%.
Poor-ish azimuth pointing performance has been noted in the course of
routine examination of the nightly pointing data.
The pointing glitches at 223 and 155.
Examination of the
track model and the
inclinometry data that created it
shows that azimuth 223 is between joints and there is no reason,
a priori, to expect trouble here. Any feature at this azimuth not
detected by the
inclinometry at the current resolution is in the middle of a track
segment. The same may be said for the glitch at 155. The
appearance of mid-segment defects would
be a worrying development, and if more widespread
would require increasing the inclinometry resolution to the 0.2 degree
level to ensure detection of all such flaws. This would increase the
time needed to take inclinometry data from the current 3 hours to
about 9 hours - a rather impractical proposition.
Yaw
I have also worried for a long time over the factor of 0.83
that we use in constructing the
yaw part of the track model. Currently
yaw = 0.83 * (LY - RY)
where LY and RY are the tilts of the left and right A-frames (in
arcseconds), although the
basis for this value is less than certain.
The current
data offer the first opportunity to fully explore the impact of
this factor on the final product. To this end,
track models were created from the inclinometry data of 980224
with various and separate factors for each of LY and RY
i.e.
yaw = fL*LY + fR*RY
It was found that a value of m_daz of 1.00 (+- 0.01) was achieved when
fL = 1.21 and fR = -1.21, both accurate to about 0.01.
With these new
values, the shorter datasets (for 3c273 and 3c279) give m_daz = 0.92 and 0.95,
respectively, which, given that the errors on m_daz and the scatters of
the azimuth residuals about the lines remain unchanged, still imply
`efficiencies' of 100%, within the errors. Meanwhile, the rms scatters in
(daz_obs - daz_pre) become
Source az range N ------------- rms scatter --------------
(daz_obs - daz_pre) (del_obs - del_pre)
3c273 133 - 234 73 1.6 1.2
3c273 215 - 234 20 1.5 0.9
3c279 215 - 234 27 1.4 0.6
Overall, such changes, and the accompanying consistency, seem
like an improvement,
and I intend testing a model using fL = -fR = 1.21 on
980410 .
An alternative suggested by
the dissociation of the left A-frame tilt from the calculation of pitch
is that fL = 0. Varying fR to achieve m_daz = 1.00 from the
3c273 data suggests that fR = -1.6, but this also increases the
scatter to 2.2". Using this value of fR on the smaller (3c273 and 3c279)
datasets gives m_daz = 0.73 +- 0.21 and 0.52 +- 0.19, respectively,
with similarly large scatters, so the entire exercise does not support
this option.
The effect of fL = -fR = 1.21 on allsky pointing data
It's always difficult to go backwards from observed pointing data to
corrections to the track model, partly because the data are logged at the
end of the pointing experiment rather than in the middle, which gives
a more representative `azimuth', but mainly because any corrections
that could be applied would be only to those azimuths at which
observations were made - and this is a very small subset of the azimuths
forming the track model. The best that can be hoped for is that
a prospective track model be tested against a pointing dataset, to see
if the overall residuals are reduced (improved).
The 32 RxA2 data of Feb 24th and the 69 SCUBA data of the 25th and 26th
were analysed.
Their basic statistics are shown below, together with the azimuth
performance that would be expected if a model based on fL = - fR = 1.21
had been used instead of that based on fL = -fR = 0.83 :
dataset FE N fL rms daz rms del
980224 A2 32 0.83 2.2 2.0
1.21 3.2
980225-26 S 69 0.83 1.5 1.9
1.21 2.3
This part of the analysis does not support changing fL from 0.83
to 1.21.
Conclusions
If the
980410 experiments do not
lead to a much improved pointing performance, the data above must be
used, as is, to determine the extent of any increase in efficiency
following the Azimuth Track Improvements Project.
The results from the
1995 work were that the track model was efficient at the 100%
mark +- 10-20% , whereas the above data suggest that this
has improved, typically to the 5-10% level.
It may be that the structure of these experiments, with their
supporting inclinometry from the previous night, allows better
results, and it may be that the
980410 results will provide an even better
track model. But, with the exception of unexplained,
unexpected glitches , often with amplitudes of 5", it seems
reasonable to claim that the inclinometry and track model
provide a description of the track irregularities accurate to 5-10% :
a factor of ~2 better than the performance reported in
1995 .
Iain Coulson
08 April 1998
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