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Analysis of inversion errors of ionospheric radio occultation

机译:电离层无线电掩星的反演误差分析

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The retrieved electron density profile of ionospheric radio occultation (RO) simulation data can be compared with the background model value during the simulation and the inversion error can be obtained exactly. This paper studies the inversion error of ionospheric RO through simulation. The sources of the inversion errors are analyzed. The impacts of measurement errors, such as the errors in phase measurements and satellite orbits, are very small and can be neglected. The approximation of straight-line propagation introduces errors at the height of the F1 layer under solar maximum condition. The spherical symmetry approximation of the electron density distribution is found to be the main source of the inversion error. The statistical results reveal some characteristics of the inversion errors. (1) The relative error increases with enhanced solar activity. (2) It is larger in winter than in equinox season, and it is smallest in summer. (3) For all seasons, it is smaller at middle latitude than at other latitudes. (4) For all seasons and geomagnetic latitudes, it is smaller at daytime than at other times. The NmF2 of the ROs from COSMIC are compared with the measurements of ionosondes, and the relative differences show the same dependencies on season, geomagnetic latitude and local time, as the relative errors of the simulated ionospheric ROs.
机译:在模拟过程中,可以将电离层无线电掩星(RO)模拟数据的检索到的电子密度分布与背景模型值进行比较,从而可以准确地获得反演误差。本文通过仿真研究了电离层反演的反演误差。分析了反演误差的来源。诸如相位测量和卫星轨道误差之类的测量误差的影响很小,可以忽略不计。在太阳最大条件下,直线传播的近似值会在F1层的高度引入误差。发现电子密度分布的球对称近似是反演误差的主要来源。统计结果揭示了反演误差的一些特征。 (1)相对误差随着太阳活动的增强而增加。 (2)冬季比春分季节大,夏季最小。 (3)在所有季节,中纬度要比其他纬度要小。 (4)对于所有季节和地磁纬度,白天白天都比其他时候小。将来自COSMIC的RO的NmF2与电离探空仪的测量值进行了比较,相对差异显示出与季节,地磁纬度和当地时间的相关性与模拟电离层RO的相对误差相同。

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