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Estimation of hmF2 and foF2 communication parameters of ionosphere F2-layer using GPS data and IRI-plas model

机译:使用GPS数据和IRI-plas模型估算电离层F2层的hmF2和foF2通信参数

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摘要

F2-layer is the most important and characteristic layer of the ionosphere in the propagation of high frequency (HF) waves due to the highest level of conductivity in the propagation path. In this study, the relation of Total Electron Content (TEC) with the maximum ionization height (hmF2) and the critical frequency (foF2) of F2 -layer are investigated within their defined parametric range using the IRI model extended towards the plasmasphere (IRI-Plas). These two parameters are optimized using daily observed GPS-TEC (IONOLAB-TEC) in an iterational loop through Non-Linear Least Squares (NLSQ) optimization while keeping the physical correlation between hmF2 and foF2 parameters. Optimization performance is examined for daily (24-hour) and hourly TEC optimizations separately. It is observed that hourly TEC optimization produces results with much smaller estimation errors. As a result of the hourly optimization, we obtain the hourly hmF2 and foF2 estimates as they are the optimization parameters. Obtained hmF2 and foF2 estimates are compared with the ionosonde estimates for various low, middle and high latitude locations for both quite and disturbed days of ionosphere. The results show that hmF2 and foF2 estimates obtained from IRI-Plas optimization (IRI-Plas-Opt) and ionosonde are very much in agreement with each other. These results also signify that IRI-Plas provides a reliable background model for ionosphere. With the proposed method, it is possible to build a virtual ionosonde via optimization of IRI-Plas model using the observed TEC values. © 1963-2012 IEEE.
机译:F2层是高频(HF)波传播过程中电离层最重要的特征层,这是因为传播路径中的电导率最高。在这项研究中,使用扩展到等离子层的IRI模型,在总的电子含量(TEC)与F2层的最大电离高度(hmF2)和临界频率(foF2)之间的关系进行了研究。 Plas)。在保持hmF2和foF2参数之间的物理相关性的同时,通过非线性最小二乘(NLSQ)优化在迭代循环中使用每日观察的GPS-TEC(IONOLAB-TEC)对这两个参数进行优化。每天(24小时)和每小时TEC优化分别检查优化性能。可以看出,每小时TEC优化产生的结果的估计误差要小得多。每小时优化的结果是,我们获得了每小时hmF2和foF2估算值,因为它们是优化参数。将电离层相当大和受干扰日的各种低,中和高纬度位置获得的hmF2和foF2估计值与离子探空仪估计值进行比较。结果表明,从IRI-Plas优化(IRI-Plas-Opt)和离子探空仪获得的hmF2和foF2估计值彼此非常吻合。这些结果也表明IRI-Plas为电离层提供了可靠的背景模型。利用所提出的方法,有可能通过使用观测到的TEC值优化IRI-Plas模型来构建虚拟离子探空仪。 ©1963-2012 IEEE。

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