Recurrent Coronal Mass Ejections and Their Geomagnetic Storms Association on 2012 January 19: Solar Surface to Upper Earth’s Atmosphere Analyses

A. Hassanin, Amira Shimeis, Hadeer F. Sabeha and F. N. Minta
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Abstract

In this study, we have conducted an analysis of space weather disruptions that occurred on 19 January 2012. Our analysis identified three coronal mass ejections (CMEs), CME1, CME2, and CME3—which were ejected at 09:48:05 universal time (UT), 14:36:05 UT, and 16:12:06 UT, respectively. Nonrecurrent disturbances in space weather, such as geomagnetic storms, result from CMEs originating from the Sun and traveling toward Earth. We assess the contribution of CME–CME interactions on 2012 January 19 and the volume emission rate of nitric oxide (NO) near the Earth's upper atmosphere in prolonging the geomagnetic disturbances observed on 2012 January 23. The findings suggest an increase in intensity at the interacting boundaries of CME1 and CME2, indicating an increase in pressure and density, leading to the compression of the magnetosphere. The 3D reconstructions of the CMEs provide evidence of unequal expansion and rotations within coronagraphic frames attributed to structural variability in the background solar wind during the eruptions. Furthermore, highlights from the in situ observations suggest that the impact of the recurrent CMEs on the geomagnetic disturbance was more pronounced within the auroral region synchronizing with a significant increase in NO volume emission rate on 2012 January 23, near the upper Earth's atmosphere. Our focus is on exploring the interactions between these CMEs to understand their potential contribution to the extended duration of the observed geomagnetic disturbance.
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2012 年 1 月 19 日的周期性日冕物质抛射及其地磁暴关联:太阳表面到地球高层大气分析
在这项研究中,我们对 2012 年 1 月 19 日发生的空间天气扰动进行了分析。我们的分析确定了三个日冕物质抛射(CMEs),即CME1、CME2和CME3,它们分别于世界标准时间(UT)09:48:05、14:36:05和16:12:06抛射。空间天气中的非周期性扰动,如地磁风暴,是由源自太阳并向地球移动的 CME 产生的。我们评估了2012年1月19日CME-CME相互作用以及地球高层大气附近一氧化氮(NO)的体积排放率对延长2012年1月23日观测到的地磁扰动的贡献。研究结果表明,CME1 和 CME2 的相互作用边界强度增加,表明压力和密度增加,导致磁层压缩。对 CME 的三维重建提供了在日冕仪框架内不平等膨胀和旋转的证据,这归因于爆发期间背景太阳风的结构变化。此外,现场观测的亮点表明,在极光区域内,周期性 CME 对地磁扰动的影响更为明显,与 2012 年 1 月 23 日地球高层大气附近 NO 体积发射率的显著增加同步。我们的重点是探索这些集合放射粒子之间的相互作用,以了解它们对观测到的地磁扰动持续时间延长的潜在贡献。
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