首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Three-dimensional estimation of electron density over Japan using the GEONET GPS network combined with SAC-C data and ionosonde measurements
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Three-dimensional estimation of electron density over Japan using the GEONET GPS network combined with SAC-C data and ionosonde measurements

机译:利用GEONET GPS网络结合SAC-C数据和离子探空仪测量,对日本的电子密度进行三维估算

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The work presented here proposes a local tomographic approach to obtain a three-dimensional description of the ionospheric electron density over Japan. To do this, a combination of GPS and ionosonde data is used in order to take advantage of the strong points of each data type. The GPS data is composed of ground and SAC-C Low Earth Orbiter observations. The ground observations correspond to measurements of 99 receivers (out of about 1000) from the dense Japanese GPS network (GEONET). SAC-C GPS limb sounding observations are processed to obtain vertical profiles of electron density. For this purpose, an improved approach of Abel inversion that considers Vertical Total Electron Content data has been used to overcome the assumption of spherical symmetry. The resulting profiles have been averaged to build a set of background profiles, which are rescaled with the ionospheric NmF2 values sounded by the Japanese network of four ionosondes and used by the tomographic algorithm to provide with vertical description of electron density. For the validation of this tomographic approach, the hourly values of NmF2 given by the four Japanese ionosondes and the vertical profiles of electron density measured by the MU Radar in Shigaraki (during the sounding campaign of November 2002) have been used. This validation with independent data shows relative discrepancies about 25% and, moreover, it shows that the use of the profiles obtained from SAC-C data offers an improvement on the dawn, dusk, and nighttime bottomside and topside estimations of the electron density with respect to the case of using the IRI model.
机译:这里提出的工作提出了一种局部层析成像方法,以获得对日本整个电离层电子密度的三维描述。为此,要结合使用GPS和离子探空仪数据,以便利用每种数据类型的优势。 GPS数据由地面和SAC-C低地球轨道器观测数据组成。地面观测值对应于来自密集日本GPS网络(GEONET)的99个接收器(约1000个)的测量值。 SAC-C GPS肢体测深观测得到处理,以获得电子密度的垂直剖面。为此,已经考虑了垂直总电子含量数据的改进的Abel反演方法被用来克服球形对称性的假设。对得到的剖面进行了平均,以建立一组背景剖面,这些剖面用由四个电离超声仪的日本网络测得的电离层NmF2值重新定标,并被层析成像算法用于提供电子密度的垂直描述。为了验证这种断层扫描方法,已使用了四个日本离子探空仪给出的NmF2的小时值和MU雷达在Shigaraki测得的电子密度的垂直剖面(在2002年11月的探测活动期间)。使用独立数据进行的验证表明相对差异约为25%,此外,它还表明,使用SAC-C数据获得的剖面可以改善黎明,黄昏和夜间的底面和顶面电子密度估计,相对于以使用IRI模型为例。

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