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An ionospheric propagation prediction method for low latitudes and mid-latitudes

机译:低纬度和中纬度的电离层传播预测方法

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An ionospheric propagation prediction method is proposed that is more responsive than current methods to the actual propagation channel of a radio wave. These other methods typically use an “average” propagation channel. The range of conditions that comprise this “average,” when considered separately, can potentially lead to quite different predictions of the propagation channel relative to the “average” alone. Thus, to the extent that a real-time trend in the propagation channel can be established, better predictions can be obtained. The proposed method obtains a real-time trend by employing a nonlinear regression analysis technique coupled together with an appropriately parameterized (empirical) ionosphere model and a ray-tracing algorithm. To test the effectiveness of this approach, we utilize measurements of group path length and elevation to several orbiting satellites from a dual-frequency (UHF/VHF) pulsed radar located near the magnetic equator. These data provide the needed statistics for the regression analysis. We then obtain satellite altitude estimations employing our method and compare these estimates to predictions obtained with a standard method. The result is an improved altitude prediction. The proposed method may also be used to obtain a better understanding of ionosphere-magnetosphere coupling, and in particular, to investigate the influence of geomagnetic activity on the low- and mid-latitude ionosphere. This is accomplished by generating parameter indices from our method and comparing these indices to solar and geomagnetic indices to see if correlations exist. To the extent that such a correlation does exist, a more accurate wave propagation prediction will result, which in turn will provide a more reliable radar tracking performance. We present comparisons between geomagnetic activity (as measured by the Kp three-hourly range index) and the parameter indices that show a weak correlation.
机译:提出了一种电离层传播预测方法,该方法比当前方法对无线电波的实际传播信道更敏感。这些其他方法通常使用“平均”传播通道。当单独考虑时,构成此“平均值”的条件范围可能会导致相对于单独的“平均值”而言,传播通道的预测完全不同。因此,在一定程度上可以建立传播信道中的实时趋势的情况下,可以获得更好的预测。所提出的方法通过采用非线性回归分析技术以及适当参数化的(经验)电离层模型和射线跟踪算法来获得实时趋势。为了测试这种方法的有效性,我们利用位于磁赤道附近的双频(UHF / VHF)脉冲雷达测量到若干轨道卫星的群路径长度和仰角。这些数据为回归分析提供了所需的统计信息。然后,我们使用我们的方法获得卫星高度估计值,并将这些估计值与使用标准方法获得的预测值进行比较。结果是改进的高度预测。所提出的方法还可用于更好地了解电离层与磁层之间的耦合,特别是研究地磁活动对低纬度和中纬度电离层的影响。这是通过根据我们的方法生成参数索引并将这些索引与太阳和地磁索引进行比较以查看是否存在相关性来实现的。在确实存在这种相关性的程度上,将得到更准确的波传播预测,这反过来将提供更可靠的雷达跟踪性能。我们介绍了地磁活动(通过Kp三个小时范围指数测得)与显示弱相关性的参数指数之间的比较。

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