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Investigation of Ionospheric Slab Thickness and Plasmaspheric TEC Using Satellite Measurements

机译:利用卫星测量研究电离层板厚和等离子层TEC

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The ionospheric slab thickness (τ) is a parameter which provides information about the nature of the distribution of ionization at a specific location and is defined as the ratio of the vertical Total Electron Content (vTEC) measured in TEC units (1 TECu = 10~(16) electrons m~(-2)) to the maximum ionospheric electron density in the F-region (NmF2). Slab thickness provides substantial information on the shape of the electron density profile as well as the neutral and ionospheric temperatures/gradients,composition and dynamics. On the other hand the electron content in the plasmasphere, termed plasmaspheric electron content (PEC) has received increasing interest in the last few years due to its significance in measuring and modeling the ionosphere to altitudes lower than GPS, in the context of transionospheric signal propagation.An investigation of the characteristics of these two parameters (r and PEC) is carried out based on 650 values of vTEC and NmF2 retrieved by a space-based technique (radio occul-tation measurements from the Constellation Observing System for Meteorology, Ionosphere, and Climate-FORMOSAT-3/COSMIC) and vTEC values based on a ground-based technique (IGS dual frequency GPS receivers facilitating monitoring of the ionosphere) taking advantage of the inherently excellent spatial coverage achieved by the satellite constellation and the relatively uniform distribution of GPS stations operating over European latitudes. To ensure that simultaneous measurements of GPS derived vTEC and COSMIC derived vTEC and NmF2 are used, the distance between the GPS stations and GPS occultation at the peak of the F layer is limited to 1° within a time interval of 5min. In addition only data during geomagnetically quiet conditions have been taken into account, as ionopsheric electron density irregularities give rise to erroneous determination of the peak density and height from GPS occultations due to significant fluctuations of the electron density profile.
机译:电离层平板厚度(τ)是一个参数,可提供有关特定位置电离分布性质的信息,并定义为以TEC单位(1 TECu = 10〜 (16)个电子m〜(-2))到F区的最大电离层电子密度(NmF2)。平板厚度提供有关电子密度分布图的形状以及中性和电离层温度/梯度,组成和动力学的大量信息。另一方面,由于在跨电离层信号传播的背景下,电离层在测量和建模低于GPS的高度方面具有重要意义,因此等离子层中的电子含量(称为等离子层电子含量(PEC))在最近几年受到了越来越多的关注。对这两个参数(r和PEC)的特性进行了研究,是基于650种通过空基技术(气象,电离层和天体星座观测系统的无线电radi合测量)获得的vTEC和NmF2值进行的。 (Climate-FORMOSAT-3 / COSMIC)和vTEC值基于地面技术(IGS双频GPS接收器有助于电离层的监测),利用了卫星星座固有的出色空间覆盖和GPS相对均匀的分布在欧洲纬度上运行的电台。为了确保同时测量GPS派生的vTEC和COSMIC派生的vTEC和NmF2,在5分钟的时间间隔内,GPS站与GPS遮挡在F层峰值之间的距离限制为1°。此外,仅考虑了地磁安静条件下的数据,因为电离子电子密度的不规则性会由于电子密度分布的显着波动而导致GPS遮掩错误地确定峰值密度和高度。

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