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Forecasting of global data-binning parameters for high-resolution empirical geomagnetic field models

机译:高分辨率经验地磁场模型的全球数据合并参数预测

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A recently developed empirical model, TS07D (http://geomag_field.jhuapl.edu/model/), has provided for the first time a realistic description of the storm-scale geomagnetic field, free from a priori assumptions about the shape of the main magnetospheric current systems. The model uses information about the global state of the magnetosphere and its solar wind driving in the form of the Sym-H index averaged over substorm scales, its time derivative, and a similarly averaged solar wind electric field. The set of global parameters is used to bin a large number of points in a historical magnetic field database and to fit the model using only a part of the database composed of points taken at times when the global data-binning parameters were close to those at the time of interest. Transition from modeling to forecasting in such models requires a modification of their data binning procedure to use only the information about the state of the solar wind and the magnetosphere prior to the time of interest. This can be done using another (forecasting) set of binning parameters, which is optimized to provide the best prediction of the original (modeling) binning set. Several sets of such parameters are investigated. It is shown that the original (modeling) set contains spurious information, which appears because of the averaging of the solar wind electric field and Sym-H index over future moments in time. As a result, the problem of the optimization of the forecasting set becomes ill-posed, and the prediction efficiency of the original binning parameters, especially the averaged time derivative of the Sym-H index, is strongly limited. The predictions are shown to be substantially improved when the forecasting set includes an exponential decay function of the solar wind electric field proposed originally by Burton et al. (1975) with the e-folding time of the order of one hour.
机译:最近开发的经验模型TS07D(http://geomag_field.jhuapl.edu/model/)首次提供了风暴规模地磁场的真实描述,而没有关于主磁场形状的先验假设。磁层电流系统。该模型使用有关磁层总体状态及其太阳风驱动的信息,其形式为在亚暴雨尺度上平均的Sym-H指数,其时间导数和类似的平均太阳风电场。全局参数集用于对历史磁场数据库中的大量点进行分箱,并且仅使用数据库的一部分拟合模型,该数据库由在全局数据分箱参数接近时的点所取的点组成感兴趣的时间。在此类模型中,从建模到预测的过渡要求修改其数据装箱过程,以仅使用有关时间之前有关太阳风和磁层状态的信息。可以使用另一组(预测)分级参数来完成此操作,该参数已优化以提供对原始(建模)分级集的最佳预测。研究了几组此类参数。结果表明,原始(建模)集包含虚假信息,该虚假信息的出现是由于未来一段时间内太阳风电场和Sym-H指数的平均值。结果,预测集的优化问题变得不适,并且原始装仓参数(尤其是Sym-H指数的平均时间导数)的预测效率受到严重限制。当预测集包含Burton等人最初提出的太阳风电场的指数衰减函数时,表明预测得到了显着改善。 (1975)的电子折叠时间大约为一小时。

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