Ionospheric Storm Caused in 2015 by Intense Geomagnetic Storms over Metro Manila, Philippines

J. Kalaw, E. Macalalad, R. M. Guido, P. Tucio, P. P. Divinagracia
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Abstract

The 2015 intense geomagnetic storms were significant event in relatively weaker solar cycle 24. In this paper, we explored the impacts of the 2015 intense geomagnetic storms and the response of the ionosphere over Metro Manila, Philippines. We obtained the data from the World Data System for Geomagnetism, Kyoto for the Kp and Dst indices; Space Radiation Lab at California Institute of Technology (SRL-CalTech) for the solar wind speed (vsw) collected by the Solar Wind Electron, Proton, and Alpha Monitor (SWEPAM) and the Advanced Composition Explorer (ACE) magnetometer for the Bz (nT) values. The total electron content was obtained from a GNSS station (PIMO) in Quezon City, Philippines, through the International Centre for Theoretical Physics (ICTP) web service. The quiet days were also acquired from the same site. Our investigation have shown that the ionosphere over the PIMO station depletes its electron density (negative storm) after reaching the minimum (during the recovery phase) and will remain for at least ~20 hours. Contrary to the CME-driven storm, the CIR-induced event in October 2015 produced negative storm (with very few and weak positive). Our results were mostly consistent with the time delay on the occurrence of a negative storm. In addition, a greater Dst minimum does not guarantee the type of storm and further analysis is required.
2015年由菲律宾马尼拉大都会强烈地磁风暴引起的电离层风暴
2015年的强地磁暴是相对较弱的第24太阳活动周的重大事件。在本文中,我们探讨了2015年强烈地磁风暴对菲律宾马尼拉大都会电离层的影响和响应。Kp和Dst指标的数据来源于京都世界地磁数据系统;由太阳风电子、质子和阿尔法监测器(SWEPAM)和高级成分探测器(ACE)磁力计收集的Bz (nT)值的太阳风速度(vsw)。总电子含量是通过国际理论物理中心(ICTP)网络服务从菲律宾奎松市的GNSS站(PIMO)获得的。安静的日子也从同一地点获得。我们的研究表明,PIMO站上空的电离层在达到最小值(在恢复阶段)后会耗尽其电子密度(负风暴),并将持续至少20小时。与cme驱动的风暴相反,2015年10月由cir引发的事件产生了负风暴(正风暴很少且微弱)。我们的结果与负风暴发生的时间延迟基本一致。此外,较大的Dst最小值并不能保证风暴的类型,需要进一步分析。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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