Huygens probe entry and descent trajectory analysis and reconstruction techniques

被引:10
作者
Atkinson, DH [1 ]
Kazeminejad, B
Gaborit, V
Ferri, F
Lebreton, JP
机构
[1] Univ Idaho, Dept Elect & Comp Engn, Moscow, ID 83844 USA
[2] Austrian Acad Sci, Space Res Inst, Dept Extraterr Phys, IWF, A-8042 Graz, Austria
[3] Observ Paris, LESIA, F-92195 Meudon, France
[4] Univ Padua, CISAS G Colombo, I-35131 Padua, Italy
[5] European Space Agcy, Res & Sci Support Dept, Estec, SCI SB, NL-2200 AG Noordwijk, Netherlands
关键词
Huygens Probe; entry and descent trajectory;
D O I
10.1016/j.pss.2004.11.005
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Cassini/Huygens is a joint National Aeronautics and Space Administration (NASA)/European Space Agency (ESA)/Agenzia Spaziale Italiana (ASI) mission on its way to explore the Saturnian system. The ESA Huygens Probe is scheduled to be released from the Orbiter on 25 December 2004 and enter the atmosphere of Titan on 14 January 2005. Probe delivery to Titan, arbitrarily defined to occur at a reference altitude of 1270 km above the surface of Titan, is the responsibility of the NASA Jet Propulsion Laboratory (JPL). ESA is then responsible for safely delivering the probe from the reference altitude to the surface. The task of reconstructing the probe trajectory and attitude from the entry point to the surface has been assigned to the Huygens Descent Trajectory Working Group (DTWG), a subgroup of the Huygens Science Working Team. The DTWG will use data provided by the Huygens Probe engineering subsystems and selected data sets acquired by the scientific payload. To correctly interpret and correlate results from the probe science experiments and to provide a reference set of data for possible "ground-truthing" Orbiter remote sensing measurements, it is essential that the trajectory reconstruction be performed as early as possible in the post-flight data analysis phase. The reconstruction of the Huygens entry and descent trajectory will be based primarily on the probe entry state vector provided by the Cassini Navigation Team, and measurements of acceleration, pressure, and temperature made by the Huygens Atmospheric Structure Instrument (HASI). Other data sets contributing to the entry and descent trajectory reconstruction include the mean molecular weight of the atmosphere measured by the probe Gas Chromatograph/Mass Spectrometer (GCMS) in the upper atmosphere and the Surface Science Package (SSP) speed of sound measurement in the lower atmosphere, accelerations measured by the Central and Radial Accelerometer Sensor Units (CASU/RASU), and the probe altitude by the two probe radar altimeters during the latter stages of the descent. In the last several hundred meters, the altitude determination will be constrained by measurements from the SSP acoustic sounder. Other instruments contributing data to the entry and descent trajectory and attitude determination include measurements of the zonal wind drift by the Doppler Wind Experiment (DWE), and probe zonal and meridional drift and probe attitude by the Descent Imager and Spectral Radiometer (DISR). In this paper, the need for and the methods by which the Huygens Probe entry and descent trajectory will be reconstructed are reviewed. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:586 / 593
页数:8
相关论文
共 30 条
[1]  
ATKINSON D, 2003, REPORT HUYGENS DESCE
[2]   The Huygens Doppler Wind Experiment - Titan winds derived from probe radio frequency measurements [J].
Bird, MK ;
Dutta-Roy, R ;
Heyl, M ;
Allison, M ;
Asmar, SW ;
Folkner, WM ;
Preston, RA ;
Atkinson, DH ;
Edenhofer, P ;
Plettemeier, D ;
Wohlmuth, R ;
Iess, L ;
Tyler, GL .
SPACE SCIENCE REVIEWS, 2002, 104 (1-2) :613-640
[3]   The Huygens Probe System Design [J].
Clausen, KC ;
Hassan, H ;
Verdant, M ;
Couzin, P ;
Huttin, G ;
Brisson, M ;
Sollazzo, C ;
Lebreton, JP .
SPACE SCIENCE REVIEWS, 2002, 104 (1-2) :155-189
[4]  
DUXBURY ED, 1998, MPFLMASIMET23EDR RDR
[5]  
DYMOND JH, 1992, VIRIAL COEFFICIENTS
[6]   The characterisation of Titan's atmospheric physical properties by the Huygens Atmospheric Structure Instrument (HASI) [J].
Fulchignoni, M ;
Ferri, F ;
Angrilli, F ;
Bar-Nun, A ;
Barucci, MA ;
Bianchini, G ;
Borucki, W ;
Coradini, M ;
Coustenis, A ;
Falkner, P ;
Flamini, E ;
Grard, R ;
Hamelin, M ;
Harri, AM ;
Leppelmeier, GW ;
Lopez-Moreno, JJ ;
McDonnell, JAM ;
McKay, CP ;
Neubauer, FH ;
Pedersen, A ;
Picardi, G ;
Pirronello, V ;
Rodrigo, R ;
Schwingenschuh, K ;
Seiff, A ;
Svedhem, H ;
Vanzani, V ;
Zarnecki, J .
SPACE SCIENCE REVIEWS, 2002, 104 (1-2) :395-431
[7]  
FULCHIGNONI M, 2002, AAS DIV PLANETARY SC, P34
[8]  
GABORIT V, 2004, SP544 PLANETARY PROB
[9]   Influence of sonic-line location on Mars Pathfinder Probe aerothermodynamics [J].
Gnoffo, PA ;
Weilmuenster, KJ ;
Braun, RD ;
Cruz, CI .
JOURNAL OF SPACECRAFT AND ROCKETS, 1996, 33 (02) :169-177
[10]   Huygens Probe aerosol collector pyrolyser experiment [J].
Israel, G ;
Cabane, M ;
Brun, JF ;
Niemann, H ;
Way, S ;
Riedler, W ;
Steller, M ;
Raulin, F ;
Coscia, D .
SPACE SCIENCE REVIEWS, 2002, 104 (1-2) :433-468