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A large‐scale view of Space Technology 5 magnetometer response to solar wind drivers

机译:太空技术5磁力计对太阳风驱动器的响应的大规模视图

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AbstractIn this data report we discuss reprocessing of the Space Technology 5 (ST5) magnetometer database for inclusion in NASA's Coordinated Data Analysis Web (CDAWeb) virtual observatory. The mission consisted of three spacecraft flying in elliptical orbits, from 27 March to 27 June 2006. Reprocessing includes (1) transforming the data into the Modified Apex Coordinate System for projection to a common reference altitude of 110 km, (2) correcting gain jumps, and (3) validating the results. We display the averaged magnetic perturbations as a keogram, which allows direct comparison of the full-mission data with the solar wind values and geomagnetic indices. With the data referenced to a common altitude, we find the following: (1) Magnetic perturbations that track the passage of corotating interaction regions and high-speed solar wind; (2) unexpectedly strong dayside perturbations during a solstice magnetospheric sawtooth oscillation interval characterized by a radial interplanetary magnetic field (IMF) component that may have enhanced the accompanying modest southward IMF; and (3) intervals of reduced magnetic perturbations or “calms,” associated with periods of slow solar wind, interspersed among variable-length episodic enhancements. These calms are most evident when the IMF is northward or projects with a northward component onto the geomagnetic dipole. The reprocessed ST5 data are in very good agreement with magnetic perturbations from the Defense Meteorological Satellite Program (DMSP) spacecraft, which we also map to 110 km. We briefly discuss the methods used to remap the ST5 data and the means of validating the results against DMSP. Our methods form the basis for future intermission comparisons of space-based magnetometer data.
机译:摘要在本数据报告中,我们讨论了对太空技术5(ST5)磁力计数据库的重新处理,以将其包含在NASA的协调数据分析网(CDAWeb)虚拟观测站中。该任务由三架在椭圆轨道上飞行的航天器组成,从2006年3月27日至6月27日。重新处理包括(1)将数据转换为改良的Apex坐标系以投影到110 akm的公共参考高度,(2)校正增益跳跃,以及(3)验证结果。我们将平均磁扰动显示为keogram,从而可以将全任务数据与太阳风值和地磁指数直接进行比较。利用参考共同高度的数据,我们发现:(1)跟踪同向相互作用区域和高速太阳风通过的磁扰动; (2)冬至磁层锯齿波振荡间隔期间的日间异常强扰动,其特征在于径向行星际磁场(IMF)分量可能增强了伴随的适度的向南IMF; (3)减少的磁扰动或“平静”的间隔,与缓慢的太阳风周期相关,穿插在变长的情节增强之中。当IMF向北或向北投射到地磁偶极子上时,这些平静最为明显。经过重新处理的ST5数据与美国国防气象卫星计划(DMSP)航天器的磁扰动非常吻合,我们也将其映射到110 km。我们简要讨论了用于重新映射ST5数据的方法以及针对DMSP验证结果的方法。我们的方法构成了未来天基磁力计数据间歇性比较的基础。

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