J. Babion et al., STRATOSPHERIC WIND SPEEDS FROM AN IR IMAGE-ANALYSIS OF THE SL-9 IMPACT REGIONS ON JUPITER, Planetary and space science, 45(10), 1997, pp. 1333
The effects of comet Shoemaker-Levy-9's impacts on Jupiter were imaged
from 16 July to 26 July 1994 through 1500 nm, 1580 nm, 1700 nm and 23
00 nm filters with the 3.5 m telescope + MAGIC camera at the Calar Alt
o Observatory, Spain. The pixel resolution of 0.32 '' corresponds to a
bout 1200 km at the sub-Earth-point on Jupiter. Good weather condition
s enabled excellent time coverage of the event. An unsharp masking ima
ge technique was applied to the images as a high-pass filter in order
to enhance the impact spot structures. For the analysis of the actual
spot geometry two kinds of maps were calculated from enhanced images:
(I) for overview purposes a projection of the southern hemisphere to a
cone and (2) for the study of details projections to a tangential pla
ne for each visible spot. From these maps we determined the sizes of t
he core and of the ejecta regions and their temporal changes during th
e first 10 days after impact. In that way we derived wind speeds and w
ind directions in the planet's stratosphere for the spots of fragments
A, C, D, E, G, H, K, L, R and QI. The stratospheric winds varied from
20 to 170 km h(-1) and are thus of the order of those in the visual c
loud deck. The wind directions varied strongly from region to region.
We have seen material of the core region being influenced by structure
s of the visual cloud deck, but a similar interrelation for the ejecta
material was not evident. We neither found impact spots from the frag
ments Q2, B, N (as seen by other observers) nor of F, P2, T, U, V. (C)
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