Great to meet you, Dr. Wooden. Thanks for sharing the IRTF image from
Nov 7th, and I look forward to your instructions on converting "lunar
geographic coordinates" to Right Ascension and Declination. Am I
correct in assuming they will appear on this forum? Or are we being
distributed via some other e-mail list?
Not being a professional astronomer I am also a bit uncertain about
the notation "g:" on your IRTF image mosaic. Does this mean
"geographic coordinates" and do they differ in some way from the usual
selenographic coordinates? I notice you have modified the values for
Schomberger C and G and Malapert K from the ones that appear in the
IAU Planetary Gazetteer. I assume this is intentional, but it seems
curious that Malapert K and Schomberger G have been given the same
values when they are indicated as being at different positions.
Also, what is the source of these numbers? Except possibly for
Faustini, they seem farther from the "correct" positions indicated in
the USGS Warped Clementine Basemap:
http://webgis.wr.usgs.gov/pigwad/down/moon_warp_clementine_750nm_basemap.htm
than do the values already appearing in the IAU Planetary Gazetteer:
http://planetarynames.wr.usgs.gov/
The approximate values I read from the USGS ULCN2005 Warped Basemap
are:
Faustini : lon = 85.26 lat= -87.18 diam = 42 km
Schomberger : lon = 24.73 lat= -76.66 diam = 85 km
Schomberger C : lon = 15.20 lat= -77.18 diam = 42 km
Schomberger G : lon = 7.23 lat= -77.02 diam = 17 km
Malapert K : lon = 5.88 lat= -78.67 diam = 36 km
unnamed crater between Schomberger C and Malapert K :
lon = 10.91 lat= -78.11 diam = 40 km
Do you have some reason to believe these are incorrect?
(the longitudes, of course, become increasingly ill-determined for
features close to the pole, and Faustini is only vaguely defined in
the Clementine mosaic)
Also, although the flier says you need 0.5 arc-sec pointing, it looks
like the IRTF telescope only detects craters to about 3-4 km diameter
(i.e., about 2 arc-sec). Is this typical? Or does the slit-viewing
imager give an incorrect impression of its performance?
Also, is it possible to rotate the IRTF slit with respect to the lunar
axis? I believe you will have a much greater chance of success if you
can orient the slit along a radial line. As the Moon's librations
change, the radial distances between landmarks varies depending on
their relative heights (which may be poorly known). Their positions
in azimuth (relative to the lunar polar axis) are little affected by
height differences. Hence you can guess where a feature will be in
azimuth much better than in radius.
Finally, I seem to recall that earlier this year NASA/JPL announced a
soon-to-be-released detailed three-dimensional Goldstone radar model
of the lunar south polar region, and perhaps Kaguya and Chang'e-1 are
working on similar things. By the time of the LCROSS impact,
shouldn't it be possible to predict the expected relationships between
lunar surface features as seen from any site using these?
Thanks again,
-- Jim