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Magnetic ground survey of Slovakia for the 2007.5 epoch – accuracy of geomagnetic elements distribution maps

机译:斯洛伐克2007.5年的磁性地面调查-地磁元素分布图的准确性

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Magnetic ground or repeat station surveys are performed to determine the geomagnetic field (GMF) spatial distribution, which is of great importance for scientific purposes as well as for many applications, for instance the aerial navigation. In for the information about the GMF distribution to be complete, the accuracy of the geomagnetic maps need to be known. It is a custom in the papers dealing with magnetic surveys that the precision of the instruments employed for the measurements are listed there. However, such information is not sufficient to answer the question about the quality of the geomagnetic maps because our experience shows that the spatial variations at a distance of several kilometers often exceed the precisions of the instruments. In the paper we proposed a simple method for the evaluation of the accuracy of the GMF distribution maps. We applied it to the maps which were the results of the magnetic ground survey carried out in Slovakia in the 2007.5 epoch. The method is based on the following procedure which is accomplished for each observation point of the magnetic ground survey network: A single point drops out of the data base, then the map is generated in a standard way, whereupon the observed value of the geomagnetic element for the dropped out observation point is compared with the value of the geomagnetic element which is determined from the map. Thus the image of the accuracy of the complete map can be tagged together for the surveyed territory
机译:进行磁性地面或重复站勘测以确定地磁场(GMF)空间分布,这对于科学目的以及许多应用(例如空中导航)都非常重要。为了使有关GMF分布的信息完整,需要知道地磁图的准确性。在处理磁测量的论文中,习惯上列出了用于测量的仪器的精度。但是,这样的信息不足以回答有关地磁图质量的问题,因为我们的经验表明,几公里距离内的空间变化通常会超出仪器的精度。在本文中,我们提出了一种简单的方法来评估GMF分布图的准确性。我们将其应用于地图,这是2007.5年代在斯洛伐克进行的磁性地面调查的结果。该方法基于以下过程,该过程针对磁性地面测量网络的每个观测点完成:从数据库中删除单个点,然后以标准方式生成地图,从而得出地磁元素的观测值将遗漏的观测点的“地磁”值与根据地图确定的地磁元素的值进行比较。因此,可以将完整地图的准确性图像标记为被调查区域

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