在TRACERS任务上的磁性搜索线圈 (MSC)
G B Hospodarsky1, A J Carton1, R T Dvorsky1
1Department of Physics and Astronomy, University of Iowa, 203 Van Allen Hall, Iowa City, 52242 IA USA.
概括
探测器任务使用磁性搜索线圈 (MSC) 仪器来测量地球磁层尖端的波浪. 这些阿尔弗文波测量有助于确定尖端动态是否是由时间或空间重新连接引起的.
科学领域:
- 空间物理 空间物理
- 等离子体物理学的物理学
- 地质物理学 地质物理学
背景情况:
- 轨迹探测器 (TRACERS) 任务是研究地球磁层尖端的动态结构.
- 了解尖端区域对于理解太阳风和磁层之间的能量转移至关重要.
研究的目的:
- 使用磁性搜索线圈 (MSC) 仪器测量磁波组件 (1 Hz 至 1 kHz).
- 确定尖端的动态结构与时间与空间重新连接相关的程度,与TRACERS科学目标3保持一致.
主要方法:
- 使用三轴,双传感器线圈系统与反放大器连续模拟输出.
- 通过电场仪表 (EFI) 电信号处理 (ESP) 板,以每秒 2048 个样本的速度以 16 位分辨率数字采样模拟信号.
- 将采样数据传送到中央数据处理单元 (CDPU) 进行分析.
主要成果:
- 成功获得了来自磁层尖端区域的三部分磁波数据.
- 提供了高分辨率的数据,对于区分时间和空间重新连接过程至关重要.
结论:
- TRACERS MSC仪器能够为磁层研究提供必要的数据.
- 收集的波浪数据有助于研究尖端区域的重新连接动态.
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