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首页> 外文期刊>Advances in space research >Ionospheric response of equatorial and low latitude F-region during the intense geomagnetic storm on 24-25 August 2005
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Ionospheric response of equatorial and low latitude F-region during the intense geomagnetic storm on 24-25 August 2005

机译:2005年8月24日至25日强烈地磁风暴期间赤道和低纬F区的电离层响应

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摘要

In this investigation, we present and discuss the response of the ionospheric F-region in the South American and East Asian sectors during an intense geomagnetic storm in August 2005. The geomagnetic storm studied reached a minimum Dst of —216 nT at 12:00 UT on 24 August. In this work ionospheric sounding data obtained of 24, 25, and 26 August 2005 at Palmas (PAL; 10.2° S, 48.2° W; dip latitude 6.6° S), Sao Jose dos Campos (SJC, 23.2° S, 45.9°W; dip latitude 17.6° S), Brazil, Ho Chi Minh City, (HCM; 10.5° N, 106.3° E; dip latitude 2.9° N), Vietnam, Okinawa (OKI; 26.3° N, 127.8° E; dip latitude 21.2° N), Japan, are presented. Also, the GPS observations obtained at different stations in the equatorial and low-latitude regions in the Brazilian sector are presented. On the night of 24-25 August 2005, the h'F variations show traveling ionospheric disturbances associated with Joule heating in the auroral zone from SJC to PAL. The foF2 variations show a positive storm phase on the night of 24-25 August at PAL and SJC during the recovery phase. Also, the GPS-VTEC observations at several stations in the Brazilian sector show a fairly similar positive storm phase on 24 August. During the fast decrease of Dst (between 10:00 and 11:00 UT) on 24 August, there is a prompt penetration of electric field of magne-tospheric origin that result in abrupt increase (~12:00 UT) in foF2 at PAL, SJC (Brazil) and OKI (Japan) and in VTEC at IMPZ, BOMJ, PARA and SMAR (Brazil). OKI showed strong oscillations of the F-region on the night 24 August resulted to the propagation of traveling atmospheric disturbances (TADs) by Joule heating in the auroral region. These effects result a strong positive observed at OKI station. During the daytime on 25 August, in the recovery phase, the foF2 observations showed positive ionospheric storm at HCM station. Some differences in the latitudinal response of the F-region is also observed in the South American and East Asian sectors.
机译:在这项调查中,我们介绍并讨论了在2005年8月发生的强烈地磁风暴中,南美和东亚地区电离层F区的响应。在12:00 UT,研究的地磁风暴的最低Dst达到-216 nT 8月24日。在这项工作中,2005年8月24日,25日和26日在帕尔马斯(PAL; 10.2°S,48.2°W;倾角6.6°S),圣何塞多斯坎波斯(SJC,23.2°S,45.9°W)获得的电离层测深数据;北纬17.6°),巴西,胡志明市(HCM;北纬10.5°,东106.3°;北纬2.9°),越南,冲绳(OKI;北纬26.3°,东127.8°;南纬21.2) °N),日本。此外,还介绍了在巴西地区的赤道和低纬度地区的不同站点获得的GPS观测结果。在2005年8月24日至25日晚上,h'F的变化显示了从SJC到PAL的极光带电离层扰动与焦耳热相关。 foF2变化在8月24日至25日晚的PAL和SJC处于恢复期的正风暴期。此外,巴西地区几个站点的GPS-VTEC观测结果显示,8月24日的正暴风期相当相似。在8月24日Dst的快速下降期间(UT的10:00至11:00之间),镁磁层起源的电场迅速穿透,导致PAL的foF2突然增加(UT〜12:00 UT) ,SJC(巴西)和OKI(日本)以及在VTEC的IMPZ,BOMJ,PARA和SMAR(巴西)。 OKI在8月24日夜间显示F区强烈振荡,这是由于极光加热过程中焦耳加热引起的行进大气干扰(TAD)的传播。这些影响导致在冲井站观察到强烈的积极影响。在8月25日的白天,处于恢复阶段,foF2观测结果表明HCM站出现了电离层正风暴。在南美和东亚地区,F区的纬度响应也有所不同。

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