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Near Real-Time Global Plasma Irregularity Monitoring by FORMOSAT-7/COSMIC-2

机译:接近实时的全球等离子不规则监控FORMOSAT-7 / COSMIC-2

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This study presents initial results of the ionospheric scintillation in the F layer using the S4 index derived from the radio occultation experiment (RO-S4) on FORMOSAT-7/COSMIC-2 (F7/C2). With the sufficiently dense RO-S4 observations at low latitudes, it is possible to construct hourly, global scintillation maps to monitor equatorial plasma bubbles (EPBs). The preliminary F7/C2 RO-S4 during August 2019 to April 2020 show clear scintillation distributions around American and the Atlantic Ocean longitudes. The RO-S4 near Jicamarca are compared with range-time-intensity (RTI) maps of the 50 MHz radar, and the results show that the occurrence of intense RO-S4 in the range 0.125–0.5 are co-located with the bottomside of the spread-F patterns. Increases in RO-S4 at the upward phase of bottom-side oscillations is theoretically consistent with large-scale wave seeding of the EPBs. The locations and occurrences of the RO-S4 greater than 0.5 are consistent with airglows depletions from the NASA GOLD mission. Climatology analyses show that monthly occurrences of RO-S4 > 0.5 agree well with the monthly EPB occurrences in GOLD 135.6 nm image, and show a similar longitudinal distribution to that of DMSP and C/NOFS in-situ measurements. The results suggest that the RO-S4 intensities can be utilized to identify EPBs of specific scales.
机译:本研究提出了初步的结果电离层闪烁在F层使用S4指数来自无线电掩星实验(RO-S4) FORMOSAT-7 / COSMIC-2(F7 / C2)。观察在低纬度地区,它是可能的构建每小时,全球地图闪烁监控赤道等离子体泡沫(epb)。初步F7 / C2 RO-S4在2019年8月2020年4月显示明显的闪烁分布在美国和大西洋经度。与range-time-intensity 50 (RTI)的地图兆赫雷达,结果表明,发生强烈的RO-S4范围0.125 - -0.5的bottomside共存spread-F模式。向上的底边相振荡理论上符合大规模的波环境保护局的播种。出现的RO-S4大于0.5一致的思路从NASA消逝黄金的任务。每月出现RO-S4 > 0.5吻合较好每月EPB出现在黄金135.6海里图像,并显示一个类似的纵向分发给DMSP和C / nof原位测量。可以用来识别引擎组件的强度具体的尺度。

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