In situ plasma and neutral gas observation time windows during a comet flyby: Application to the Comet Interceptor mission

IF 1.8 4区 物理与天体物理 Q3 ASTRONOMY & ASTROPHYSICS Planetary and Space Science Pub Date : 2024-03-11 DOI:10.1016/j.pss.2024.105878
J. De Keyser , N.J.T. Edberg , P. Henri , H.-U. Auster , M. Galand , M. Rubin , H. Nilsson , J. Soucek , N. André , V. Della Corte , H. Rothkaehl , R. Funase , S. Kasahara , C. Corral Van Damme
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Abstract

A comet flyby, like the one planned for ESA’s Comet Interceptor mission, places stringent requirements on spacecraft resources. To plan the time line of in situ plasma and neutral gas observations during the flyby, the size of the comet magnetosphere and neutral coma must be estimated well. For given solar irradiance and solar wind conditions, comet composition, and neutral gas expansion speed, the size of gas coma and magnetosphere during the flyby can be estimated from the gas production rate and the flyby geometry. Combined with flyby velocity, the time spent in these regions can be inferred and a data acquisition plan can be elaborated for each instrument, compatible with the limited data storage capacity. The sizes of magnetosphere and gas coma are found from a statistical analysis based on the probability distributions of gas production rate, flyby velocity, and solar wind conditions. The size of the magnetosphere as measured by bow shock standoff distance is 105106  km near 1 au in the unlikely case of a Halley-type target comet, down to a nonexistent bow shock for targets with low activity. This translates into durations up to 103104 seconds. These estimates can be narrowed down when a target is identified far from the Sun, and even more so as its activity can be predicted more reliably closer to the Sun. Plasma and neutral gas instruments on the Comet Interceptor main spacecraft can monitor the entire flyby by using an adaptive data acquisition strategy in the context of a record-and-playback scenario. For probes released from the main spacecraft, the inter-satellite communication link limits the data return. For a slow flyby of an active comet, the probes may not yet be released during the inbound bow shock crossing.

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彗星飞越期间的原位等离子体和中性气体观测时间窗口:彗星拦截器任务的应用
彗星飞越,如欧空局计划的彗星拦截器飞行任务,对航天器资源提出了严格的要求。为了规划飞越期间原位等离子体和中性气体观测的时间线,必须充分估计彗星磁层和中性彗尾的大小。在给定的太阳辐照度和太阳风条件、彗星成分和中性气体膨胀速度下,飞越期间气体彗尾和磁层的大小可以通过气体产生率和飞越几何形状估算出来。结合飞越速度,可以推断出在这些区域停留的时间,并根据有限的数据存储容量为每个仪器制定数据采集计划。磁层和气体彗星的大小是根据气体产生率、飞越速度和太阳风条件的概率分布进行统计分析得出的。在哈雷型目标彗星不太可能出现的情况下,根据弓形冲击距离测量的磁层大小为 105-106 千米,接近 1 au,而在低活动性目标彗星中,则不存在弓形冲击。这意味着持续时间可达 103-104 秒。当目标被确定在距离太阳较远的地方时,这些估计值就会缩小,而当目标的活动被更可靠地预测到距离太阳较近的地方时,这些估计值就会更小。彗星拦截者主航天器上的等离子体和中性气体仪器可以在记录和回放的情况下使用自适应数据采集策略监测整个飞越过程。对于从主航天器上释放的探测器,卫星间通信链路限制了数据返回。对于慢速飞越活动彗星的情况,探测器可能还没有在入轨弓形冲击穿越期间释放。
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来源期刊
Planetary and Space Science
Planetary and Space Science 地学天文-天文与天体物理
CiteScore
5.40
自引率
4.20%
发文量
126
审稿时长
15 weeks
期刊介绍: Planetary and Space Science publishes original articles as well as short communications (letters). Ground-based and space-borne instrumentation and laboratory simulation of solar system processes are included. The following fields of planetary and solar system research are covered: • Celestial mechanics, including dynamical evolution of the solar system, gravitational captures and resonances, relativistic effects, tracking and dynamics • Cosmochemistry and origin, including all aspects of the formation and initial physical and chemical evolution of the solar system • Terrestrial planets and satellites, including the physics of the interiors, geology and morphology of the surfaces, tectonics, mineralogy and dating • Outer planets and satellites, including formation and evolution, remote sensing at all wavelengths and in situ measurements • Planetary atmospheres, including formation and evolution, circulation and meteorology, boundary layers, remote sensing and laboratory simulation • Planetary magnetospheres and ionospheres, including origin of magnetic fields, magnetospheric plasma and radiation belts, and their interaction with the sun, the solar wind and satellites • Small bodies, dust and rings, including asteroids, comets and zodiacal light and their interaction with the solar radiation and the solar wind • Exobiology, including origin of life, detection of planetary ecosystems and pre-biological phenomena in the solar system and laboratory simulations • Extrasolar systems, including the detection and/or the detectability of exoplanets and planetary systems, their formation and evolution, the physical and chemical properties of the exoplanets • History of planetary and space research
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