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Assimilation of real-time riometer measurements into models of 30?MHz polar cap absorption

机译:将实时测距仪的测量值同化到30?MHz极极吸收的模型中

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Space weather events may adversely affect high frequency (HF) radio propagation, hence the ability to provide nowcasting and forecasting of HF radio absorption is key for industries that rely on HF communications. This paper presents methods of assimilating 30?MHz radio absorption measurements into two types of ionospheric polar cap absorption (PCA) model to improve their performance as nowcasting tools. Type 1 models calculate absorption as m times the square root of the flux of solar protons above an energy threshold, E _( t ). Measurements from 14 riometers during 94 solar proton events (1995–2010) are assimilated by optimising the day and night values of m by linear regression. Further non-linear optimisations are demonstrated in which parameters such as E _( t )are also optimised and additional terms characterise local time and seasonal variations. These optimisations reduce RMS errors by up to 36%. Type 2 models incorporate altitude profiles of electron and neutral densities and electron temperatures. Here the scale height of the effective recombination coefficient profile in the D-region is optimised by regression. Furthermore, two published models of the rigidity cut-off latitude (CL) are assessed by comparison with riometer measurements. A small improvement in performance is observed by introducing a 3-h lag in the geomagnetic index K _( p )in the CL models. Assimilating data from a single riometer in the polar cap reduces RMS errors below 1?dB with less than 0.2?dB bias. However, many high-latitude riometers now provide absorption measurements in near-real time and we demonstrate how these data may be assimilated by fitting a low-order spherical harmonic function to both the measurements and a PCA model with optimised parameters.
机译:空间天气事件可能会对高频(HF)无线电传播产生不利影响,因此,对于依赖HF通信的行业,提供HF无线电吸收的临近预报和预测能力至关重要。本文介绍了将30?MHz无线电吸收测量结果同化为两种类型的电离层极性帽吸收(PCA)模型的方法,以提高其作为临近预报工具的性能。 1型模型将吸收量计算为高于能量阈值E _(t)的太阳质子通量的平方根的m倍。通过线性回归优化m的昼夜值,可以同化94个太阳质子事件(1995-2010年)中14个测距仪的测量值。进一步的非线性优化被证明,其中诸如E_(t)的参数也被优化,并且附加项表征了当地时间和季节变化。这些优化措施可将RMS误差降低多达36%。 2型模型结合了电子和中性密度以及电子温度的高度剖面。在此,通过回归优化D区域中有效重组系数分布图的刻度高度。此外,通过与测距仪的测量结果进行比较,评估了两个公开的刚度截止纬度(CL)模型。通过在CL模型中的地磁指数K _(p)中引入3小时的滞后,可以观察到性能的小幅提高。从极极帽中的单个riometer吸收数据可将RMS误差降低至1?dB以下,且偏差小于0.2?dB。但是,许多高纬度测距仪现在提供近实时的吸收测量值,并且我们演示了如何通过将低阶球谐函数拟合到测量值和具有优化参数的PCA模型来吸收这些数据。

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