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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Response of the equatorial and low-latitude ionosphere in the Indiansector to the geomagnetic storms of January 2005
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Response of the equatorial and low-latitude ionosphere in the Indiansector to the geomagnetic storms of January 2005

机译:印度洋地区的赤道和低纬度电离层对2005年1月的地磁风暴的响应

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摘要

The equatorial and low-latitude ionospheric response to three moderate geomagneticstorms (17, 18, and 22 January) during the period from 16 to 23 January 2005 isinvestigated in the context of development/inhibition of the Equatorial IonizationAnomaly (ETA) and the subsequent occurrenceonoccurrence of Equatorial SpreadF (ESF) irregularities on these days. The study is carried out using the Total ElectronContent (TEC) measured with the GPS receivers along the --,80°E longitude sector andthe F-layer bottom height obtained from the Ionosonde located over the dip equatoriallocation of Trivandrum (8.5°N, 77°E, dip latitude '0.5°N) in India. It is observed that, forthe storms on days 17 and 22, the development of the anomaly was inhibited, probablydue to the westward disturbance dynamo electric fields. Subsequently, the post sunsetenhancement in the vertical drift of the equatorial F region was also inhibited significantlycompared to the quiet day pattern and, as anticipated, no ESF was observed on thesedays. A large vertical drift of the equatorial F region followed by nearly simultaneousonset of weak ESF was observed on day 18. The late development of the EIA on this daycould be due to the eastward prompt penetration electric field associated with thesouthward turning of the interplanetary magnetic field. Also, strong and distinct F3 layerappeared for a short time in the morning, reappeared later in the noon time, and thenquickly ascended to the topside ionosphere during the main phase of the storm on day 18.
机译:在发展/抑制赤道电离异常(ETA)以及随后发生/发生的背景下,研究了2005年1月16日至23日对3次中等地磁风暴(1月17日,18日和22日)的赤道和低纬电离层响应这些天未发生赤道SpreadF(ESF)异常情况。该研究使用GPS接收器沿--80°E经度扇区测得的总电子含量(TEC)和从位于Trivandrum赤道赤道上方的离子探空仪获得的F层底部高度(8.5°N,77 °E,倾角纬度'0.5°N)在印度。可以看出,对于第17天和第22天的暴风雨,异常的发展受到了抑制,这可能是由于向西扰动发电机电场所致。随后,与安静日模式相比,赤道F区垂直漂移的日落后增强也被显着抑制,并且正如预期的那样,这些天没有观察到ESF。在第18天,赤道F区出现了较大的垂直漂移,随后几乎同时出现了弱的ESF。EIA在这一天的后期发展可能是由于与行星际磁场向南旋转有关的东向快速穿透电场。同样,强而独特的F3层在早上的短时间内出现,在午后又出现,然后在第18天的暴风雨主要阶段迅速上升到电离层的顶部。

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