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Validation of the space weather modeling framework using observations from CHAMP and DMSP

机译:利用CHAMP和DMSP的观测结果验证空间天气建模框架

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The Space Weather Modeling Framework (SWMF) is a flexible framework for space weather simulation, which can couple magnetosphere and ionosphere processes. This work compares ionospheric outputs from SWMF with magnetic and plasma observations from CHAMP and DMSP satellites under both quiet and storm conditions, emphasizing the dependence of the model's performance for various magnetic local times, solar wind conditions, and seasons. The model predicts the potential better in the dawn-dusk sector then in the noon-midnight sector. For field-aligned currents (FACs) the model performs better on the dayside than on the nightside. In addition, there is a trend toward unsatisfactory behavior in the model as solar activity increases. The model more accurately corresponds to observations during quiet times than disturbed periods. During storms the model FACs tend to locate at ∼4° MLat more poleward than the observations. Our analysis has revealed that the model performance depends strongly on the seasons. The model underestimates the cross polar cap potential (CPCP) by about ∼50% in the summer hemisphere while overestimating it by ∼50% in the winter hemisphere. The model calculates the difference between the winter and summer hemisphere CPCP on the order of a factor of 2.5, while DMSP data show that the actual factor is around 1.3. These results reveal that the ionospheric modeling subsets lack appropriate seasonal dependence.
机译:空间天气建模框架(SWMF)是用于空间天气模拟的灵活框架,可以耦合磁层和电离层过程。这项工作将SWMF的电离层输出与CHAMP和DMSP卫星在安静和暴风雨条件下的磁和等离子体观测结果进行了比较,强调了该模型对各种磁当地时间,太阳风条件和季节的性能依赖性。该模型预测,黎明黄昏地区的潜力要好于午夜时段。对于场对准电流(FAC),该模型在白天比在夜间表现更好。另外,随着太阳活动的增加,模型中的行为趋向于不令人满意。该模型比干扰期更准确地对应于安静时间的观测值。在暴风雨期间,模型FAC的位置往往比观测值更偏向约4°ML。我们的分析表明,模型的性能很大程度上取决于季节。该模型在夏季半球低估了约28%的跨极极电势(CPCP),而在冬季半球高估了约50%的跨极极电势。该模型计算出冬季和夏季半球CPCP的差异约为2.5倍,而DMSP数据显示实际系数约为1.3。这些结果表明,电离层模拟子集缺乏适当的季节依赖性。

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