Baker Daniel N, Dewey Ryan M, Lawrence David J, Goldsten John O, Peplowski Patrick N, Korth Haje, Slavin James A, Krimigis Stamatios M, Anderson Brian J, Ho George C, McNutt Ralph L, Raines Jim M, Schriver David, Solomon Sean C
Laboratory for Atmospheric and Space Physics University of Colorado Boulder Colorado USA.
The Johns Hopkins University Applied Physics Laboratory Laurel Maryland USA.
J Geophys Res Space Phys. 2016 Mar;121(3):2171-2184. doi: 10.1002/2015JA021778. Epub 2016 Mar 18.
The MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) mission to Mercury has provided a wealth of new data about energetic particle phenomena. With observations from MESSENGER's Energetic Particle Spectrometer, as well as data arising from energetic electrons recorded by the X-Ray Spectrometer and Gamma-Ray and Neutron Spectrometer (GRNS) instruments, recent work greatly extends our record of the acceleration, transport, and loss of energetic electrons at Mercury. The combined data sets include measurements from a few keV up to several hundred keV in electron kinetic energy and have permitted relatively good spatial and temporal resolution for many events. We focus here on the detailed nature of energetic electron bursts measured by the GRNS system, and we place these events in the context of solar wind and magnetospheric forcing at Mercury. Our examination of data at high temporal resolution (10 ms) during the period March 2013 through October 2014 supports strongly the view that energetic electrons are accelerated in the near-tail region of Mercury's magnetosphere and are subsequently "injected" onto closed magnetic field lines on the planetary nightside. The electrons populate the plasma sheet and drift rapidly eastward toward the dawn and prenoon sectors, at times executing multiple complete drifts around the planet to form "quasi-trapped" populations.
前往水星的“信使号”(MErcury Surface, Space ENvironment, GEochemistry, and Ranging,缩写为MESSENGER)任务提供了大量关于高能粒子现象的新数据。借助“信使号”高能粒子谱仪的观测结果,以及X射线谱仪、伽马射线和中子谱仪(GRNS)记录的高能电子数据,近期的研究极大地拓展了我们对水星高能电子加速、传输和损失情况的记录。这些综合数据集涵盖了从几keV到几百keV的电子动能测量值,并且对于许多事件而言,具备了相对良好的空间和时间分辨率。我们在此聚焦于GRNS系统所测量的高能电子爆发的详细特性,并将这些事件置于水星的太阳风及磁层强迫的背景下进行考量。我们对2013年3月至2014年10月期间高时间分辨率(10毫秒)的数据进行了研究,这有力地支持了以下观点:高能电子在水星磁层的近尾区域被加速,随后被“注入”到行星夜侧的封闭磁力线上。这些电子填充了等离子体片,并迅速向东朝着黎明和午前扇区漂移,有时会围绕行星进行多次完整的漂移,从而形成“准捕获”粒子群。