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首页> 外文期刊>Annales Geophysicae >Daily variation at three Antarctic geomagnetic observatories within the polar cap
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Daily variation at three Antarctic geomagnetic observatories within the polar cap

机译:极地帽内三个南极地磁观测站的每日变化

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摘要

In this work we present a statistical analysis of the diurnal variation as observed at three Antarctic observatories located at different positions within the polar cap during the year 2006. Data used for the analysis are from the Italian geomagnetic observatory at Mario Zucchelli Station (formerly Terra Nova Bay, geographic latitude 74.7° S, corrected geomagnetic latitude 80.0° S), from the French-Italian observatory at Concordia Station (75.1° S, 88.9° S) and from the French observatory at Dumont D'Urville (66.7° S, 80.4° S), which are located in pairs at the same geographic and corrected geomagnetic latitude; such a position allows to distinguish whether the geographic or the geomagnetic reference system is better suitable to describe the observed phenomena at so high latitudes. The peculiarities of the daily variation as observed during this year and its relation with the observatory location and magnetospheric and interplanetary conditions were analysed. Data were also studied taking into account different Lloyd seasons. The results indicate that the 24-h variation is quite persistent, but its amplitude strongly depends on season and global geomagnetic activity: indeed, it almost vanishes during local winter for quiet geomagnetic conditions; this reduction is more evident at the stations closer to the geographic pole, where the solar radiation reduction during winter is more dramatic. The Interplanetary Magnetic Field orientation has been found to be important in that the north-south and the east-west components control the amplitude and the diurnal pattern of the variation, respectively.
机译:在这项工作中,我们对2006年在极地帽内不同位置的三个南极观测站观测到的昼夜变化进行了统计分析。用于分析的数据来自马里奥·祖凯利站(以前叫Terra Nova)的意大利地磁观测站。海湾,地理纬度为74.7°S,校正后的地磁纬度为80.0°S),来自Concordia站的法意天文台(75.1°S,88.9°S)和来自法国杜蒙特杜维尔的天文台(66.7°S,80.4) °S),成对放置在相同的地理和校正的地磁纬度上;这样的位置可以区分地理参考系统还是地磁参考系统是否更适合描述如此高纬度的观测现象。分析了今年观测到的每日变化的特点及其与天文台位置,磁层和行星际状况的关系。还根据不同的劳埃德季节对数据进行了研究。结果表明,24小时变化是相当持久的,但其幅度在很大程度上取决于季节和全球地磁活动:实际上,在安静的地磁条件下,它在当地冬季几乎消失了。这种减少在靠近地理极点的站点更为明显,那里冬季的太阳辐射减少更为显着。发现星际磁场方向很重要,因为南北分量和东西向分量分别控制振幅和日变化模式。

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