Swarm 星座观测到的电离层顶部上游波驱动的压缩 Pc3-4 脉动的一致性

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2024-09-03 DOI:10.1029/2024JA032502
Chunyu Xu, Hermann Lühr, Chao Xiong, Fengjue Wang, Yunliang Zhou
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引用次数: 0

摘要

在这项研究中,我们利用对蜂群 A 和蜂群 B 的磁场测量,详细分析了频率在 16 至 100 mHz 之间的超低频压缩波。这些波被认为是由前震区的过程驱动的,随后被称为上游波(UWs)。我们开发了一种用于识别上游波事件的自动检测算法,并将其应用于 "蜂群 "磁场测量。与以往的研究不同,我们利用反向旋转的 Swarm 星座来研究大尺度均匀波场。只有来自 Swarm A 和 B 卫星的 B 场振荡符合以下标准,才可用于 UWs 分析:(a) 高度相关,归一化相关系数 (Cc) 大于 0.9;(b) 两次观测之间的偏移小于 3 秒;(c) 在纬度和/或经度上相距 90°。通过这一程序,我们在两个航天器的磁场记录中总共识别出 2018-2023 年间含有 UWs 的 577 个轨道。第一步,我们检查了纬度相距较大的 UW 探测器之间的相位偏移。两个反向旋转的航天器可以利用多普勒效应来检查电离层高度上可能存在的 UW 传播。虽然个别事件显示出波向南北传播的迹象,但平均而言,没有发现系统性的运动。同样,还检查了波向正午或偏离正午的可能运动。通过分析更大纵向间隔的同步观测数据,也几乎没有发现东西方向的相位差。此外,通过评估统计结果,似乎出现了平均微小的局部时间效应,表明波浪平均在上午较早到达,而在傍晚较晚到达。
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Coherence of Compressional Pc3-4 Pulsation Driven by Upstream Waves in Topside Ionosphere Observed by the Swarm Constellation

In this study, we presented a detailed analysis of ultralow frequency compressional waves with frequencies ranging from 16 to 100 mHz by using magnetic measurements of Swarm A and B, when the two spacecraft were flying in a counter-rotating configuration. These waves are assumed to be driven by processes in the fore-shock region and subsequently termed as upstream waves (UWs). An automatic detection algorithm for identifying UW events has been developed and applied to the Swarm magnetic measurements. Different to previous studies we take advantage of the counter-rotating Swarm constellation to investigate the large-scale homogeneous wavefield. Only B-field oscillations from both Swarm A and B satellites satisfy the following criteria are accepted for UWs analysis: (a) highly correlated with normalized correlation coefficient (Cc) larger than 0.9; (b) shifted by less than 3 s between observations; (c) separated up to 90° in latitude and/or longitude. By this procedure we have identified from the years 2018–2023 in total 577 orbits containing UWs in the magnetic recordings of both spacecraft. In the first step, we checked phase shifts between UW detections at large latitudinal separation. The two counter-rotating spacecraft allowed to make use of the Doppler effect to check the possible propagation of UWs at ionospheric altitude. Although individual events show signs of north-south wave propagation, on average no systematic motion could be found. Similarly, possible wave motions toward or away from noon hours have been checked. By analyzing the simultaneous observations at larger longitudinal separation, also hardly any phase differences are identified in the east-west direction. Further by evaluating the statistical results, a mean tiny local time effect seems to emerge, indicating on average an earlier arrival of the waves in the morning and later in the evening hours.

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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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