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The author observed the impact of comet Shoemaker-Levy 9 on Jupiter by near-infrared wavelength using the 188-cm telescope, with the near-IR camera OASIS, for Okayama Astrophysical Observatory during July 15-24, 1994, and succeeded the detections of the impacts of the fragments C, D, and K. The observational results with good time resolution showed the complicated behavior of the impact radiation and some stages of the impact phenomena; the two short precursors, PC1 and PC2, and the long lasting main event, and the shoulder.

Those phenomena were also observed for other impacts.

The author attempted to synthesize the overview of the impact phenomena.

The spacecraft Galileo detected the impacts of the SL9 fragments. Comparing ground-based observations with the detections by Galileo, it is shown that the PC1 is the radiation by entry of the fragment into the high altitude atmosphere.

The PC2 timings are related with the impact geometries. As a result of the explosion of the cometary fragment, the expanding and rising plume was ejected.

The vertical eject velocity of the plume was more 10 km s-1, and the plume rose to the height of Earth-line of sight within one minute. Thus thermal radiation from the hot plume was detected at some ground-based infrared observations as the PC2.

From 6 minutes after the impact, the main event started. The cause of the main event is debatable subject. Many researchers proposed the heating by the splash back of the plume as a cause of the main event. However the author do not sustain this theory by two reasons. The first reason is that the estimated temperatures of the impact radiator continued to decrease even in first half of the main event. The temperature increased from 10 minutes after the impact, which was after the peak of the main event. The second one is that the center position of the radiation did not change between before and after the main event start, but started to move southward at the speed of 4 km s-1 at 10 minutes after the impact again. Both the reasons mean that the splash back of the plume started at 10 minutes after the impact.

Therefore the author proposes dust grain formation theory as a cause of the main event. The formation of dust grain enhances the optical depth of the plume, and then enhances both the thermal radiation and the reflected sunlight.

The formation of dust grain in the plume at the start of the main event is consistent with the HST and other visible observations. The plume motion is modeled as simple ballistic motion. By comparing this ballistic model with the OAO observation of the K impact, the plume temperatures are estimated and shown to be consistent with other observations. The composition of the dust is probably silicate.

It is clear that more detailed analysis and precise modeling are needed in order to obtain the conclusion on the impact phenomena. It is left as a future work.

77

Acknowledgments

I am deeply grateful to Mr. Hitoshi Hasegawa of ASTEC, Inc., for co-research on the SL9 impact with him, without it I would never have achieved this study.

I would like to thank greatly to Dr. Jun-ichi Watanabe of the public information office, N AOJ for the organization of the OAO /OASIS observation and helpful discussions.

I express my thanks to Prof. Hideo Maehara, the director of the OAO, and all the staffs of OAO and the OASIS group for supports to the observation. In particular, fr. Atsushi Mori of Department of Astronomy, University of Tokyo, made some comments on reductions of the OASIS data, which are very valuable.

I am grateful to Prof. Kazuhiro Sekiguchi of NAOJ, who presented the data of the SAAO observations, and to Dr. David Crisp and Dr. Vikki Meadows of JPL, who presented the data of color temperature by AAT/IRIS, and to Mr. Naotaka Yamamoto of Department of Physics, Science University of Tokyo, for support on reductions and analyses. Thanks are due to Prof. Masahisa Yanagisawa of University of Electro-Communications, Dr. Toshiko Takata and Prof. Sho Sasaki of Geological Institute, University of Tokyo, and all the members of PLANET mailing-list and Planetary and Lunar Astronomical Network of Japan for helpful comments and discussions. I also thanks Miss Sumiko Harasawa for advices of English expressions.

Finally, I express my thanks deeply to Prof. Saburo Miyahara of Depart­

ment of Earth and Planetary Sciences, Kyushu University for his guidances and critical readings of the manuscript, and to the members of the laboratory for supports on my study, in particular, to Dr. Takahiro Iwayama of Department of Control Engineering and Science, Kyushu Institute of Technology for many supports and courtesies.

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