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Ionospheric Estimation over Japan Based on GNSS Regression Models and GEONET Data

机译:基于GNSS回归模型和地理数据数据的日本电离层估计

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In this paper, we present an ionospheric estimation method based on GNSS Regression models (abbreviated by GR models) and show to derive the ionospheric delay (or advance) local model in the sky over Japan using the Gps Earth Observation NETwork (GEONET) data provided from the Geographical Survey Institute (GSI) of Japan. First we introduce the very powerful models of observables in GPS/GNSS; called GR models. By applying GR models, we have already developed the precise point positioning (PPP) algorithm and the very precise point positioning (VPPP) algorithm with multiple antennas. These positioning algorithms achieved the positioning accuracy in decimeter level. These algorithms do not require the realtime transmitted information such as from WAAS etc. By showing the GR models for GNSS observables in the case of known positions (in the reference stations), we derive a method to estimate the ionospheric delays (or advances) as well as the so-called integer ambiguities contained in L1 and L2 band carrier-phase data at the reference stations. Then we emphasize the importance to estimate integer ambiguities of their own receivers at the reference stations. Further, we derive the method of estimating the local model with power series for the vertical total electron content (VTEC) at the ionospheric pierce points in the ionospheric single-layer model by using GPS receiver’s data at many reference stations. Finally the local estimated model of the vertical TEC in the sky over Japan using GEONET data is shown comparatively with applying Klobuchar’s model and with the Global Ionosphere Maps (GIMs) provided by the International GNSS Service (IGS).
机译:在本文中,我们提出了一种基于GNSS回归模型的电离层估计方法(GR模型缩写),并显示使用提供的GPS地球观测网络(GeOnet)数据来导出天空中的电离层延迟(或前进)本地模型来自日本地理调查研究所(GSI)。首先,我们在GPS / GNSS中介绍了非常强大的观察模型;叫GR模型。通过应用GR模型,我们已经开发了具有多个天线的精确点定位(PPP)算法和非常精确点定位(VPPP)算法。这些定位算法实现了减距水平的定位精度。这些算法不需要从WAAS等的实时传输信息。通过在已知位置(在参考站中的情况下)的GNSS可观察到的GR模型,我们推导了一种估计电离层延迟(或前进)的方法。以及参考站的L1和L2频段载波相位数据中包含的所谓整数歧义。然后我们强调重要性来估计他们自己的接收者的整数含量在参考站。此外,我们通过使用GPS接收器的数据在许多参考站中,通过使用GPS接收器的数据,从电离层单层模型中的电离层皮带处的垂直总电子含量(VTEC)估算局部模型的方法。最后,使用GeOnet数据的日本天空中垂直TEC的垂直TEC的局部估计模型相对显示,使用国际GNSS服务(IGS)提供的全球电离层地图(GIM)。

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