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首页> 外文期刊>Advances in space research >Traveling ionospheric disturbances observed at South African midlatitudes during the 29-31 October 2003 geomagnetically disturbed period
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Traveling ionospheric disturbances observed at South African midlatitudes during the 29-31 October 2003 geomagnetically disturbed period

机译:2003年10月29日至31日在南非中纬度观测到的电离层行进干扰

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摘要

This paper presents traveling ionospheric disturbances (TIDs) observations from GPS measurements over the South African region during the geomagnetically disturbed period of 29-31 October 2003. Two receiver arrays, which were along two distinct longitudinal sectors of about 18°-20° and 27°-28° were used in order to investigate the amplitude, periods and virtual propagation characteristics of the storm induced ionospheric disturbances. The study revealed a large sudden TEC increase on 28 October 2003, the day before the first of the two major storms studied here, that was recorded simultaneously by all the receivers used. This pre-storm enhancement was linked to an X-class solar flare, auroral/magnetospheric activities and vertical plasma drift, based on the behaviour of the geomagnetic storm and auroral indices as well as strong equatorial electrojet. Diurnal trends of the TEC and foF2 measurements revealed that the geomagnetic storm caused a negative ionospheric storm; these parameters were depleted between 29 and 31 October 2003. Large scale traveling ionospheric disturbances were observed on the days of the geomagnetic storms (29 and 31 October 2003), using line-of-sight vertical TEC (vTEC) measurements from individual satellites. Amplitude and dominant periods of these structures varied between 0.08-2.16 TECU, and 1.07-2.13 h respectively. The wave structures were observed to propagate towards the equator with velocities between 587.04 and 1635.09 m/s.
机译:本文介绍了2003年10月29日至31日在地磁扰动期间在南非地区进行GPS测量得出的电离层扰动(TIDs)观测结果。两个接收器阵列分别沿两个不同的纵向扇区分别为18°-20°和27为了研究风暴诱发的电离层扰动的幅度,周期和虚拟传播特性,使用了-28°。该研究表明,在这里研究的两次大风暴中的第一场暴风雨发生的前一天,即2003年10月28日TEC突然急剧增加,所有使用的接收器同时记录了这一变化。暴风雨前的这种增强与X级太阳耀斑,极光/磁层活动和垂直等离子漂移有关,这是基于地磁暴和极光指数以及强赤道电喷的行为。 TEC和foF2的日变化趋势表明,地磁风暴​​引起了负电离层风暴。这些参数在2003年10月29日至31日之间被耗尽。在地磁风暴发生的当天(2003年10月29日至31日),观测到了大规模的电离层扰动,使用了单个卫星的视线垂直TEC(vTEC)测量。这些结构的振幅和主导周期分别在0.08-2.16 TECU和1.07-2.13 h之间变化。观察到波结构以587.04和1635.09 m / s之间的速度向赤道传播。

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