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Online computation of International Reference Ionosphere Extended to Plasmasphere (IRI-Plas) model for space weather

机译:太空天气的国际参考电离层扩展到等离子层(IRI-Plas)模型的在线计算

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摘要

Ionosphere is the most challenging part of Space Weather with its spatio-temporal variability and dispersive nature. Ionospheric models are very important in reducing positioning error in GNSS system. International Reference Ionosphere (IRI) is an empirical, deterministic and climatic model of ionosphere up to 2000 km in height. Recently, IRI Extended to Plasmasphere (IRI-Plas) model has been developed to extend the interest region of IRI to the GPS orbital height of 20,000 km. Both IRI and IRI-Plas provide ionospheric parameters such as electron density, electron and ion temperatures according to their height profiles. In order to update the model to current ionospheric conditions, IRI-Plas can input F2 layer critical frequency (foF2), maximum ionization height (hmF2), and also Total Electron Content (TEC). Online IRI-Plas is developed for the ionospheric community to run multiple tasks at various locations, dates and times with optional foF2, hmF2 and TEC inputs in a user-friendly manner. In this paper, we are going to present the capabilities of the Online IRI-Plas service and provide some comparisons between IRI-Plas outputs and ionosonde measurements. The comparison between online IRI-Plas foF2 outputs and ionosonde foF2 measurements indicates that the model with TEC input can significantly improve the representation of the current ionospheric state, which is very successful especially in the geomagneti-cally disturbed days.
机译:电离层具有时空变异性和分散性,是空间天气最具挑战性的部分。电离层模型对于减少GNSS系统中的定位误差非常重要。国际参考电离层(IRI)是一个经验,确定性和气候模型,最高可达200​​0 km。最近,已经开发了IRI扩展到等离子层(IRI-Plas)模型,以将IRI的关注区域扩展到20,000 km的GPS轨道高度。 IRI和IRI-Plas都根据其高度分布提供电离层参数,例如电子密度,电子和离子温度。为了将模型更新为当前的电离层条件,IRI-Plas可以输入F2层临界频率(foF2),最大电离高度(hmF2)以及总电子含量(TEC)。在线IRI-Plas是为电离层社区开发的,可以通过用户友好的方式使用可选的foF2,hmF2和TEC输入在不同的位置,日期和时间运行多个任务。在本文中,我们将介绍在线IRI-Plas服务的功能,并提供IRI-Plas输出和离子探空仪测量值之间的一些比较。在线IRI-Plas foF2输出和电离探空foF2测量结果之间的比较表明,带TEC输入的模型可以显着改善当前电离层状态的表示,这是非常成功的,尤其是在受到地磁影响的日子。

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  • 来源
    《大地测量与地球动力学(英文版)》 |2018年第5期|347-357|共11页
  • 作者单位

    Department of Electrical and Electronics Engineering, Hacettepe University, Beytepe, Ankara, 06800, Turkey;

    IZMIRAN, Troitsk, Moscow, 108840, Russian Federation;

    Department of Electrical and Electronics Engineering, Hacettepe University, Beytepe, Ankara, 06800, Turkey;

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