Regional ionosphere modeling using spherical cap harmonics and empirical orthogonal functions over Iran

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• 作者：Mir Reza Ghaffari Razin ; Behzad Voosoghi
• 关键词：Ionosphere electron density ; Spherical cap harmonics ; Empirical orthogonal functions ; GPS ; IRI2012
• 刊名：Acta Geodaetica et Geophysica
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：52
• 期：1
• 页码：19-33
• 全文大小：
• 刊物主题：Geophysics/Geodesy;
• 出版者：Springer Netherlands
• ISSN：2213-5820
• 卷排序：52

文摘

The ionosphere is the ionized part of the upper region of the atmosphere extending from 60 to 1500 km above the earth’s surface. In this layer, free electrons are produced during the interaction of extreme ultra violet and x-ray radiation with the upper neutral atmosphere. Knowledge of the ionospheric electron density distribution is important for scientific studies and practical applications. In this paper, a new computerized ionospheric tomography reconstruction technique is developed to estimate electron density profiles over Iran. In this method, a functional based model is used to represent the electron density in space. The functional based model uses empirical orthogonal functions and spherical cap harmonics to describe the vertical and horizontal distribution of the electron density, respectively. The degree and the number of basis functions are chosen so that, the relative error of results is minimized. For this purpose, ionosonde observations (Lat. = 35.73°, Lon. = 51.38°) at 2007.04.03 is used. To apply the method for constructing a 3D-image of the electron density, GPS measurements of the Iranian permanent GPS network (at 2012/08/11) has been used. The modeling region is between 24 to 40 N and 44 to 64 W. The result of 3D-model has been compared to that of the international reference ionosphere model 2012 (IRI-2012). The analysis conducted in this paper indicates that the choice of spherical cap harmonics to 3 (K_max = 3) and empirical orthogonal function in 3 (Q = 3), the regional reconstructed error is less than 36 %. The results show the advantages of this method in modeling of the ionosphere electron density on local and regional scales.