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首页> 外文期刊>Current Journal of Applied Science and Technology >Classification of Days Using Locally GeneratedMagnetic Indices from Magnetic DataAcquisition System (Magdas) Ground BasedObservatories at Three (3) Nigerian Stations
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Classification of Days Using Locally GeneratedMagnetic Indices from Magnetic DataAcquisition System (Magdas) Ground BasedObservatories at Three (3) Nigerian Stations

机译:使用来自三(3)个尼日利亚站点的磁数据采集系统(Magdas)地面观测站的本地生成的磁指数来分类天数

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Investigation has been done concerning the mitigation of geomagnetic storm (a type of space weather that has the potential to cause damage across the globe with a single event) using locally generated magnetic Indices obtained from geomagnetic data from ground based Magdas magnetometers to classify the data into quiet and disturbed days thereby deducing the possible state of radio communications propagation over Nigeria. Physical mechanisms responsible for the characteristics of the ionosphere were identified. K (an index which measures the magnetic perturbations of the planetary field) and A (a linear measure of the Earth's field that provides a daily average level for geomagnetic activity) geomagnetic indices were generated locally using a simple algorithm and appropriate computer code, from MAGDAS magnetometers located at Abuja (9o 40’N, 7o 29’E), Ilorin (8o30’N, 4o33’E) and Lagos (6o27’N, 3o23’E) in Nigeria for the period 2006 – 2011 were used as the basis for the classification. Results showed that 31.85% of the days were found to be quiet while 39.36% of the days were found to be disturbed. The observed variations in the geomagnetic field responsible for the characteristics of the ionosphere over Nigeria comes probably from two principal sources, namely, transient variations - those generated by atmospheric processes such as ultraviolet radiation from the sun and partly by secular variations, which are due to internal disturbances within the Earth. Variations in the geomagnetic field are thus found to be responsible for the characteristics of the Ionosphere.
机译:已经进行了有关减轻地磁风暴(一种可能通过一次事件在全球范围内造成损害的太空天气)的研究,该研究使用了从地面Magdas磁力计的地磁数据获得的本地生成的磁指数来将数据分类为安静而受干扰的日子,从而推论出尼日利亚境内无线电通信传播的可能状态。确定了造成电离层特征的物理机制。使用MAGDAS,使用简单的算法和适当的计算机代码在本地生成了K(用于测量行星磁场的磁扰动的指数)和A(用于提供每日平均水平的地磁活动的线性测量)的地磁指数。以2006年至2011年期间位于尼日利亚阿布贾(9o 40'N,7o 29'E),Ilorin(8o30'N,4o33'E)和拉各斯(6o27'N,3o23'E)的磁力计为基础用于分类。结果表明,有31.85%的日子是安静的,而有39.36%的日子是被打扰的。观察到的造成尼日利亚电离层特征的地磁场变化可能来自两个主要来源,即瞬态变化-由大气过程(如来自太阳的紫外线辐射)产生的瞬态变化,以及部分由于长期变化而产生的瞬态变化。地球内部的内部干扰。因此,发现地磁场的变化是造成电离层特征的原因。

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