Observations of Comet 19P/Borrelly by the Miniature Integrated Camera and Spectrometer Aboard Deep Space 1

Author:

Soderblom L. A.1,Becker T. L.1,Bennett G.1,Boice D. C.2,Britt D. T.3,Brown R. H.4,Buratti B. J.5,Isbell C.1,Giese B.6,Hare T.1,Hicks M. D.5,Howington-Kraus E.1,Kirk R. L.1,Lee M.5,Nelson R. M.5,Oberst J.6,Owen T. C.7,Rayman M. D.5,Sandel B. R.4,Stern S. A.8,Thomas N.9,Yelle R. V.4

Affiliation:

1. United States Geological Survey, 2255 North Gemini Drive, Flagstaff, AZ 86001, USA.

2. Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78238, USA.

3. Department of Geological Sciences, University of Tennessee, 306 Geological Sciences Building, Knoxville, TN 37996, USA.

4. Department of Planetary Science, Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA.

5. Jet Propulsion Laboratory (JPL), California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.

6. DLR Institute of Space Sensor Technology and Planetary Exploration, Rutherfordstrasse, 2D-12489 Berlin, Germany.

7. Institute for Astronomy, University of Hawaii, 2680 Woodlawn Drive, Honolulu, HI 96822, USA.

8. Department of Space Studies, Southwest Research Institute, 1050 Walnut Street No. 426, Boulder, CO 80302, USA.

9. Max-Planck-Institut für Aeronomie, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.

Abstract

The nucleus of the Jupiter-family comet 19P/Borrelly was closely observed by the Miniature Integrated Camera and Spectrometer aboard the Deep Space 1 spacecraft on 22 September 2001. The 8-kilometer-long body is highly variegated on a scale of 200 meters, exhibiting large albedo variations (0.01 to 0.03) and complex geologic relationships. Short-wavelength infrared spectra (1.3 to 2.6 micrometers) show a slope toward the red and a hot, dry surface (≤345 kelvin, with no trace of water ice or hydrated minerals), consistent with ∼10% or less of the surface actively sublimating. Borrelly's coma exhibits two types of dust features: fans and highly collimated jets. At encounter, the near-nucleus coma was dominated by a prominent dust jet that resolved into at least three smaller jets emanating from a broad basin in the middle of the nucleus. Because the major dust jet remained fixed in orientation, it is evidently aligned near the rotation axis of the nucleus.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference28 articles.

1. H. U. Keller et al. Astron. Astrophys. 187 807 (1987).

2. Comets are grouped into dynamical classes according to their orbital characteristics. According to (28) known comets now include 211 short-period (SP) comets (also known as Jupiter-family) with periods less than about 30 years 37 intermediate-period (IP) comets (also known as Halley-family) with periods of about 30 to 200 years and 1166 long-period (LP) comets with periods >200 years. The source region of the SP comets is thought to be the Kuiper Belt a torus-shaped region just beyond the orbit of Neptune where they formed. LP comets come from the Oort cloud a roughly spherical distribution of comets at the extreme limits of our solar system (a few tens of thousands of AU from the Sun). It is generally believed that Oort cloud comets originated in the Uranus-Neptune region and were then gravitationally scattered into the Oort cloud whereas IP comets formed in the same region but were scattered into the region of the Kuiper Belt.

3. M. F. A'Hearn et al. Icarus 118 223 (1995).

4. M. D. Rayman et al. Acta Astron. 47 475 (2001).

5. The deep space 1 extended mission

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