Full text: Technical Commission IV (B4)

  
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B4, 2012 
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia 
hardware coordinates disagreed with the NAC average values 
by more than 50 m. The cause of these outlier estimates is under 
investigation. 
2.2 Elevation 
The elevation for each object was derived using 2 m per pixel 
digital terrain models (DTMs) produced from NAC stereo 
images (Tran, 2010) tied to LOLA altitude tracks, which are 
accurate in elevation to +2-5 m for the Apollo sites. At the 
LRRR sites, we modified the DTM elevation values by taking 
the difference in elevation between the NAC DTM’s LRRR 
elevation and the elevation from laser ranging (Williams 2010), 
and applying that difference to the whole NAC DTM. The 
vertical offsets at all three LRRR sites were <2 m. 
To calculate each object's coordinates, the corresponding image 
is projected on a sphere with a radius equal to the object's 
elevation. This strategy mitigates parallax errors from inexact 
surface intersections due to small errors in spacecraft position or 
pointing knowledge. To determine the coordinates of a pixel, 
the instrument line of sight for that pixel is intersected with a 
shape model. If that model is a DTM rather than a sphere, then 
the differences in elevation around the correct point can 
magnify ephemeris errors. This problem primarily affects the 
longitude of coordinates in off-nadir images, but there are many 
off-nadir images of the Apollo sites, as they were high-priority 
targets that were imaged on many orbits that did not pass 
directly over the sites. 
2.3 Ground Coordinates 
To compute the ground coordinates of an object from a line and 
sample pair in an non-map-projected NAC image, we used the 
CAMPT function in the Integrated System for Imagers and 
Spectrometers (ISIS) (Anderson, 2004), which in turn uses 
routines in the NASA Navigation and Ancillary Information 
Facility's (NAIF) SPICE Toolkit. CAMPT calculates ground 
coordinates from pixel coordinates using the relevant kernel 
files, which define the absolute locations and orientations of the 
spacecraft, instrument, and target. The two key time dependent 
kernels in this case are the spacecraft kernel (SPK), which 
contains the spacecraft position relative to the Moon for a given 
time period, and the camera kernel (CK), which contains 
orientation information for the spacecraft and instruments over 
time. CAMPT uses the appropriate kernels to determine the 
instrument location and pointing when each pixel was imaged, 
and intersects the line of sight for that pixel with a shape model 
of the Moon to determine the ground coordinates of that pixel. 
After preparing an appropriate shape model as described earlier, 
the largest remaining position uncertainty, on the order of 50 m, 
is due to temperature dependent NAC pointing errors. These 
errors were corrected using temperature- and slew-dependent 
CK files that our team developed, which reduce the average 
absolute positioning error to £15 m in both latitude and 
longitude (Speyerer, 2012). This correction modifies the camera 
pointing relative to the spacecraft body based on the 
temperature of the structure to which the NACs are mounted, 
and the angle the spacecraft is slewed towards or away from the 
Sun. The latter may be a proxy for differential heating across 
the mounting points, although the exact physical mechanism is 
unknown. See Speyerer et al. (this volume) for further 
discussion. 
2.3.1  LRRR Sites: At the Apollo 11, 14, and 15 sites, the 
LRRRs enable accurate control of the spacecraft pointing (Table 
1). For each image, we updated the camera pointing using the 
DeltaCK function of ISIS, which updates the cross-track and 
down-track components of the camera pointing to align the 
image with a known point, assuming the estimated spacecraft 
position is correct. We then collected and averaged the locations 
of each object from these corrected images. This method 
restricted the usable images to those where the LRRR was 
visible, but dramatically reduced the variation (to +2 m at most) 
in calculated hardware positions as compared to the sites 
without LRRRs (Table 2). 
  
  
  
  
  
  
  
  
  
  
  
Object Latitude Longitude Radius (m) 
All LRRR 0.673440 23.473073 1735472.7 
Al4 LRRR -3.644170 | 342.521352 1736336.1 
A1S LRRR 26.133396 3.628507 1735477.3 
Lunokhod 1 38.315158 | 324.992036 1734928.7 
Lunokhod 2 25.832307 30.922149 1734639.0 
  
Table 1: Laser ranging derived coordinates for the five lunar 
retroreflectors, from Williams (2008) (Apollos and Lunokhod 2) 
and Murphy (2011) (Lunokhod 1). These values, and all others 
reported in this paper, are in mean Earth/polar axis coordinates. 
2.3.2 Sites with no LRRR: At the Apollo 12, 16, and 17 
sites, there is no reference point with coordinates known to 
similar or better accuracy than the NAC pixel size (the ALSEP 
central station positions are only known to +30 m (Davies and 
Colvin, 2000)). Thus, at these locations, hardware coordinates 
were calculated by using the average latitude and longitude 
from all NAC images in which each object is visible (Table 2). 
3. RESULTS 
The calculated positions for each object, along with the 
uncertainties in each measurement, are shown in Table 2. 
4. DISCUSSION 
41.1 Accuracy of Davies and Colvin estimates: The 
difference between coordinates derived by Davies and Colvin 
(2000) and the those reported here were generally close to the 
reported uncertainties from Davies and Colvin: 5 m for the 
Apollo 14 and 15 ALSEPs, and 30 m for the Apollo 12, 16, and 
17 ALSEPs. No error estimates were given for the LMs, but 
their coordinates were also within 30 m of the NAC 
coordinates. The worst lateral offset was the Apollo 16 LM, at 
29 m southeast of the Davies and Colvin coordinates. Their 
reported elevations, however, were high by 40 m at every site 
without an LRRR, which is larger than the maximum vertical 
error reported by Davies and Colvin for the VLBI data. A 
possible source for some of this error is inaccuracy in Davies 
and Colvin vertical and horizontal positions of the reference 
ALSEPs at Apollos 14 and 15 relative to the LRRRs. At Apollo 
14, the ALSEP position was off by 6 m in latitude, longitude, 
and altitude, although the Apollo 15 ALSEP was only off by 3 
m in longitude. We note that the published USGS maps (All, 
A12, A14) and sketch maps in the mission preliminary science 
reports (A15, A16, A17), which were used by Davies and 
Colvin to locate the LMs relative to the ALSEPS, are good to 
within 10-20 m over the 60-200 m distance between the ALSEP 
and LM at each site. 
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