Aj. Friedson et al., THERMAL INFRARED LIGHTCURVES OF THE IMPACT OF COMET SHOEMAKER-LEVY-9 FRAGMENT-R, Geophysical research letters, 22(12), 1995, pp. 1569-1572
The impact of fragment R was observed at thermal infrared wavelengths
of 7.85, 10.3 and 12.2 mu m from the NASA/Infrared Telescope Facility
on July 21 UT, using the MIRAC2 mid-infrared array camera. Thermal emi
ssion at the three wavelengths was sampled sequentially using a 1.8% c
ircular variable filter, with an average time interval of 17 seconds b
etween observations at different wavelengths. Continuous imaging of Ju
piter in this mode began at 5:08 UT and extended to 5:55 UT. We presen
t calibrated lightcurves for the three wavelengths. Clear evidence for
enhanced emission from the impact region first appears at 5:41 UT, wi
th the peak in emission at all three wavelengths occurring similar to
3.5 minutes later. The information content of the data is presented in
terms of plots of the product of emissivity times angular size versus
source temperature for each wavelength. Assuming that the peak in the
lightcurves is due to rotation of the hot impact site into view from
Earth, we estimate a diameter of similar to 1900 km for the source emi
tting area at 5:44:30 UT and estimate a lower limit on the source temp
erature at this time of similar to 1350 K. This lower limit drops to 8
00 K if the diameter of the emitting region was actually a factor of t
wo larger.