ASTEROID-243 IDA - GROUNDBASED PHOTOMETRY AND A PRE-GALILEO PHYSICAL MODEL

被引:38
作者
BINZEL, RP
SLIVAN, SM
MAGNUSSON, P
WISNIEWSKI, WZ
DRUMMOND, J
LUMME, K
BARUCCI, MA
DOTTO, E
ANGELI, C
LAZZARO, D
MOTTOLA, S
GONANOBEURER, M
MICHALOWSKI, T
DEANGELIS, G
THOLEN, DJ
DIMARTINO, M
HOFFMANN, M
GEYER, EH
VELICHKO, F
机构
[1] ASTRON OBSERV,S-75120 UPPSALA,SWEDEN
[2] OBSERV HELSINKI,SF-00014 HELSINKI,FINLAND
[3] UNIV ARIZONA,LUNAR & PLANETARY LAB,TUCSON,AZ 85721
[4] PHILLIPS LAB,LIGE,KIRTLAND AFB,NM 87117
[5] OBSERV PARIS,F-92195 MEUDON,FRANCE
[6] GERMAN AEROSP RES ESTAB,O-1199 BERLIN,GERMANY
[7] ADAM MICKIEWICZ UNIV POZNAN,ASTRON OBSERV,PL-60286 POZNAN,POLAND
[8] ESTEC,ESA,DEPT SPACE SCI,DIV PLANETARY & SPACE SCI,2200 AG NOORDWIJK,NETHERLANDS
[9] INST ASTRON,HONOLULU,HI 96822
[10] OSSERV ASTRON TORINO,I-10025 PINO TORINESE,ITALY
[11] UNIV BONN,OBSERV HOHER LIST,D-54550 DAUN,GERMANY
[12] KHARKOV ASTRON OBSERV,310022 KHARKOV,UKRAINE
关键词
D O I
10.1006/icar.1993.1129
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Groundbased photometric observations of asteroid 243 Ida over seven apparitions from 1980 to 1993 allow us to derive a model for its spin vector and shape prior to the August 1993 encounter by the Galileo spacecraft. Two equally likely solutions for the spin vector are at ecliptic coordinates (1950) λp1 = 73, βp1 = -53 or λp2 = 254, βp2 = -55 with an uncertainty of ± 10° in each coordinate. Ida's low orbital inclination restricts the available aspect angles for Earth-based observers so that the spin vector ambiguity cannot be resolved. We offer predictions for the flyby geometry for both solutions, where the Galileo spacecraft images will resolve this ambiguity easily. Ida's rotation is retrograde with a sidereal period of 4.633632 ± 0.000007 hr. Assuming a triaxial ellipsoid model, we estimate axial ratios of a/b = 1.82 ± 0.10 and b/c = 1.15 ± 0.10. The morphology of the observed lightcurves suggest that Ida has a nonuniform albedo distribution, but we cannot completely rule out observational uncertainties or simplifying model assumptions (e.g., convex shape, geometric scattering) as sources for this suggestion. It is not possible to predict uniquely the distribution of any such albedo variegation. © 1993 by Academic Press, Inc.
引用
收藏
页码:310 / 325
页数:16
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