电离层
地磁风暴
地球磁场
风暴
气泡
大气科学
气象学
地球物理学
地质学
环境科学
物理
机械
磁场
量子力学
作者
Xiankang Dou,Guozhu Li,Shun‐Rong Zhang,Lianhuan Hu,Guozhong Dai,Biqiang Zhao,Yuichi Otsuka,Xiukuan Zhao,Hongqiang Xie,Xuehui Li,Baiqi Ning,Libo Liu,Atsuki Shinbori,Michi Nishioka,Septi Perwitasari
摘要
Abstract An unseasonal equatorial plasma bubble (EPB) event occurred in the East/Southeast Asian sector during the geomagnetic storm on 1 December 2023, causing strong amplitude scintillations from equatorial to middle latitudes. Based on the observations from multiple instruments over a large latitudinal and longitudinal region, the spatial features of the super EPB were investigated. The EPB developed vertically at a fast rising speed ∼470 m/s over the magnetic equator and extended to a very high middle latitude more than 40°N, despite that the storm intensity was not very strong with the minimum SYM‐H index −132 nT. In the zonal direction, the super EPB covered over a specific region ∼95–140°E, where the local sunset roughly coincided with southward turning of interplanetary magnetic field (IMF) Bz component. Before the onset of the super EPB, significant upward plasma drift up to ∼110 m/s was observed over the magnetic equator, which could amplify the growth rate of Rayleigh‐Taylor instability and lead to the generation of the super EPB. The significant drift was likely caused by eastward penetration electric field (PEF) due to sharp southward turning of IMF Bz. The local time of storm onset and duration of IMF Bz southward turning during the storm main phase may partly determine the onset region and zonal coverage of the EPB.
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