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Dawn Mission to Vesta and Ceres
Authors:C. T. Russell  F. Capaccioni  A. Coradini  M. C. De Sanctis  W. C. Feldman  R. Jaumann  H. U. Keller  T. B. McCord  L. A. McFadden  S. Mottola  C. M. Pieters  T. H. Prettyman  C. A. Raymond  M. V. Sykes  D. E. Smith  M. T. Zuber
Affiliation:1. IGPP & ESS, UCLA, Los Angeles, CA, 90095-1567, USA
2. INAF, Via del fosso del Cavaliere, Rome, 00133, Italy
3. IFSI, Via del fosso del Cavaliere, Rome, 00133, Italy
4. IAFS, Via del fosso del Cavaliere, Rome, 00133, Italy
5. LANL, MS D466, NIS-1, Los Alamos, NM, 87545, USA
6. DLR Rutherfordstr 2, 12489, Berlin, Germany
7. MPAE, 37191, Katlenburg-Lindau, Germany
8. University of Hawaii, 2525 Correa Rd., Honolulu, HI, 96822, USA
9. University of Maryland, College Park, MD, 20742, USA
10. Brown University, Providence, RI, 02912, USA
11. JPL, 4800 Oak Grove Dr, Pasadena, CA, 91109, USA
12. PSI, 1700 East Fort Lowell, Suite 106, Tucson, AZ, 85719-2395, USA
13. GSFC, MC 920, Greenbelt, MD, 20771, USA
14. MIT, Cambridge, MA, 02139, USA
Abstract:The initial exploration of any planetary object requires a careful mission design guided by our knowledge of that object as gained by terrestrial observers. This process is very evident in the development of the Dawn mission to the minor planets 1 Ceres and 4 Vesta. This mission was designed to verify the basaltic nature of Vesta inferred both from its reflectance spectrum and from the composition of the howardite, eucrite and diogenite meteorites believed to have originated on Vesta. Hubble Space Telescope observations have determined Vesta’s size and shape, which, together with masses inferred from gravitational perturbations, have provided estimates of its density. These investigations have enabled the Dawn team to choose the appropriate instrumentation and to design its orbital operations at Vesta. Until recently Ceres has remained more of an enigma. Adaptive-optics and HST observations now have provided data from which we can begin to confidently plan the mission. These observations reveal a rotationally symmetric body with little surface relief, an ultraviolet bright point that can be used as a control point for determining the pole and anchoring a geographic coordinate system. They also reveal albedo and color variations that provide tantalizing hints of surface processes.
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