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On the smooth surface of the northern bow shock of Mars, based on Mars Global Surveyor's measurements

机译:根据火星全球测量师的测量,在火星北部弓形冲击的光滑表面上

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摘要

A very smooth and time-invariable bow shock of Mars is revealed using Mars Global Surveyor's data. The bow-shock position has been identified using magnetic and electron flux data obtained by the Magnetometer and Electron Reflectometer (MAG/ER) experiment aboard Mars Global Surveyor, in the time period between days 87 and 255 of 1998. From the magnetic field and the electron flux measurements, 148 bow-shock crossings were detected, concentrated mostly on the northern hemisphere of the planet. With these results, a 3D configuration of the bow shock is constructed and presented. The results show that part of the observed bow shock is a surprisingly smooth surface. It is possible that the bow shock is smooth only in the northern hemisphere, since the southern surface is characterized by local magnetic anomalies. Its real shape can only be revealed in a 3D representation in the planetary centered solar ecliptic coordinate system and questions the theoretically expected variation of the bow shock.
机译:火星全球测量师的数据显示出火星非常平稳且不随时间变化的弓形冲击。利用1998年第87天至255天之间的时间,由Mars Global Surveyor上的磁力计和电子反射计(MAG / ER)实验获得的磁通量和电子通量数据,可以确定船首的位置。电子通量测量结果表明,发现了148次弓震过境,主要集中在地球的北半球。有了这些结果,就可以构建并提供弓形冲击的3D配置。结果表明,观察到的弓形冲击的一部分是出乎意料的光滑表面。弓激波可能仅在北半球是平滑的,因为南部表面的特征是局部磁异常。它的真实形状只能在以行星为中心的太阳黄道坐标系中以3D形式显示,并质疑弓形冲击在理论上的预期变化。

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  • 来源
    《Solar Physics》 |2001年第1期|191-200|共10页
  • 作者

    N. Sergis; X. Moussas;

  • 作者单位

    Department of Astrophysics Astronomy and Mechanics Faculty of Physics National University of Athens Panepistimiopolis;

    Department of Astrophysics Astronomy and Mechanics Faculty of Physics National University of Athens Panepistimiopolis;

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  • 正文语种 eng
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