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A Physics-Based Data Assimilation Model for the High-Latitude Ionosphere: Importance of Data Assimilation Technique in Determining the Model Drivers

机译:高纬度电离层的基于物理学的数据同化模型:数据同化技术在确定模型驱动程序时的重要性

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The high-latitude ionosphere is a very dynamic region in the solar-terrestrial system. The constantly existing weather disturbances in the region can adversely affect numerous military and civilian systems and the accurate specification and forecasting of its plasma and electrodynamic structures have fundamental space weather significance. Presently, most of the space-weather models use limited observations and/or indices to define a set of empirical drivers for physical models to move forward in time. Since the empirical drivers have a "climatological" nature and there are significant physical inconsistencies among various empirical drivers due to independent statistical analysis of different observational data or even different inputs to the drivers, the specifications of high-latitude environment from these models can not truthfully reflect the weather features and unrealistic small- and large-scale structures could be produced. UtahStateUniversity has developed a data assimilation model for the high-latitude ionospheric plasma dynamics and electrodynamics to overcome these hurdles. With a set of physical models and an ensemble Kalman filter, the model can determine the drivers that are most truthful to the real space environment by ingesting data from multiple observations, including magnetic perturbation from more than 100 ground-based magnetometers, magnetic measurements of IRIDIUM satellites, SuperDARN line-of-sight velocity, and in-situ drift velocity measured by DMSP satellites. As a result, the model can realistically capture the small- and large-scale plasma structures and sharp electrodynamic boundaries, thus providing a more accurate picture of the high-latitude space weather. In this paper, we describe how the model determines the most truthful drivers and quantitatively demonstrate the differences between the model results of directly using empirical drivers and those of using the drivers that are determined by an ensemble Kalman filter. With these results, we then elucidate the importance of data assimilation for accurate specification and forecasting of space weather.
机译:高纬度电离层是太阳能系统中的一个非常动态的区域。该地区的不断现有的天气紊乱可能对众多军事和民用系统产生不利影响,并且准确的规格和预测其等离子体和电动结构具有基本的空间天气意义。目前,大多数空间天气模型都使用有限的观察和/或指标来定义一组实证驱动因素,用于及时向前移动。由于经验司机具有“气候学”的性质,并且由于对不同观察数据的独立统计分析或对驱动程序的不同意见,这些模型的高纬度环境的规格,各种实证驱动因素之间存在显着的身体不一致。反映天气特征,可以生产天气特征和不切实际的小和大规模结构。犹他州大学已经开发了一种用于高纬度电离层等离子体动力学和电动动力学的数据同化模型,以克服这些障碍。与一组物理模型和一个集合卡尔曼滤波,该模型可确定通过摄取来自多个意见,包括来自超过100基于地面的磁力磁扰动,铱的磁测量数据是最真实的实际空间环境中的驱动程序DMSP卫星测量的卫星,Superdarn视线速度和原位漂移速度。结果,该模型可以在实际捕获小型和大规​​模的等离子体结构和尖锐的电动边界,从而提供更准确的高纬度空间天气的图像。在本文中,我们描述了模型如何确定最诚实的驱动程序,并定量地展示直接使用经验驱动程序的模型结果与使用由合奏卡尔曼滤波器确定的驱动程序的模型结果之间的差异。通过这些结果,我们阐明了数据同化的重要性,以便准确规范和空间天气预报。

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