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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Generation of Proxy GIM-TEC for Extreme Storms Before the Era of GNSS Observations
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Generation of Proxy GIM-TEC for Extreme Storms Before the Era of GNSS Observations

机译:代的代理GIM-TEC极端风暴GNSS时代之前的观察

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For the first time, we reconstructed global distribution of both the total electron content disturbance W index and TEC values for eight extreme storms (Dst < ?250 nT) occurred before the epoch of GNSS observations in solar cycle 22. We created a model based on superposed epoch analysis of the training set of GIM-W maps of nine SC23 extreme storms. Global GIM-W index maps are calculated from 15-min UPC GIM-TEC (UQRG) as the logarithmic deviation of instantaneous TEC from the monthly median GIMMTEC empirical model. We introduced the storm phase metrics for main and recovery phases of the positive ionosphere disturbance (the WU-index), the negative disturbance (the WL-index) and the ring current (the Dst-index). The probabilistic forecasting model (Pmodel) for SC22 GIM-Wx maps is developed based on GIM-W maps of the SC23 training set. The storm phase distribution Φx for the eight SC22 extreme storms is calculated from the proxy time shift (lag) of peak WUmax and WLmin relative to Dstmin. Proxy GIM-TECx maps are calculated by adjusting the GIM-MTEC median to the GIM-Wx prediction. Validation of the technique based on data of UPC and JPL for four intense ionospheric storms showed a root-mean-square error less than 3 TECU. The proposed technique can be applied for both the past and future forecasting of GIM-W index and GIM-TEC maps.
机译:第一次,我们重建全球分布的总电子含量干扰W指数和TEC值8极端风暴(Dst < ? 250元)发生之前GNSS观察太阳周期22的时代。我们创建了一个模型基于叠加的时代训练集的分析GIM-W的地图九SC23极端风暴。计算从下半场UPC GIM-TEC (UQRG)瞬时TEC的对数偏差从每月平均GIMMTEC实证模型。我们介绍了风暴阶段为主要指标和恢复阶段的积极的电离层干扰(WU-index),负的干扰(WL-index)和环电流(Dst-index)。模型(Pmodel) SC22 GIM-Wx地图基于GIM-W SC23训练集的映射。八SC22风暴阶段分布Φx极端风暴从代理计算时间转变(滞后)的峰值WUmax WLmin相对Dstmin。调整GIM-Wx GIM-MTEC值预测。数据UPC和喷气推进实验室四个强烈的电离层风暴显示均方根误差小于3为一例。GIM-W的过去和未来预测指数和GIM-TEC地图。

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