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首页> 外文期刊>Annales Geophysicae >Can the comprehensive model phase 4 (CM4) predict the geomagnetic diurnal field for days away from quiet time?
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Can the comprehensive model phase 4 (CM4) predict the geomagnetic diurnal field for days away from quiet time?

机译:综合模型第4阶段(CM4)是否可以在远离安静时间的几天内预测地磁昼夜场?

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摘要

The most recent comprehensive model (CM4) of the geomagnetic field (Sabaka et al., 2004) has been used in conjunction with geomagnetic ground observatory station data to analyse and study the geomagnetic diurnal variation field for days away from quiet time and the CM4 prediction for these times. Even though much has been learnt about many components of the geomagnetic field, the diurnal variation field behaviour for days away from quiet time (moderately disturbed time) has not been intensively studied. Consequently, we analyse these, and the predictive ability of the CM4 for ground variations, and whether the CM4 prediction of the diurnal variation (whether at quiet time or away from quiet time) is valid outside the period of reference that from which the data were used in modelling. In carrying out the study, we compared the observatory station data and the CM4 prediction directly. Using the CM4 code, well-characterised internal and magnetospheric components were subtracted from the data, plots and global maps of the residual field generated and then compared with the CM4 to see how well the model performed in predicting the data at moderately disturbed time (Kp <= 5). The results show that the CM4 is valid and produces useful predictions outside the period covering the timespan of the model and during moderately disturbed time, despite the lack of active data in the original model dataset. The model predictability of the data increases as we move to higher spherical harmonic degree truncation, as the model-data misfit is reduced, but with increased roughness as a result of small-scale features incorporated. The observed results show that this relationship between the increase in spherical harmonic degree truncation and reduction in misfit can be restricted by data quality or quantity and global coverage or spread.
机译:最近的地磁场综合模型(CM4)(Sabaka et al。,2004)已与地磁地面观测站数据结合使用,以分析和研究远离安静时间和CM4预测几天的地磁日变化场在这些时候。尽管已经对地磁场的许多组成部分学到了很多,但对于远离静默时间(中度扰动时间)的几天的日变化场行为尚未进行深入研究。因此,我们分析了这些数据,并分析了CM4对地面变化的预测能力,以及CM4对日变化的预测(无论是在静默时间还是远离静默时间)在参考数据的参考期间之外均有效。用于建模。在进行研究时,我们直接比较了天文台的数据和CM4的预测。使用CM4代码,从生成的剩余场的数据,图和全局图中减去特征明确的内部和磁层分量,然后与CM4进行比较,以查看模型在中等扰动时间(Kp <= 5)。结果表明,尽管原始模型数据集中缺少活动数据,但CM4是有效的,并且可以在覆盖模型时间段的期间之外以及中等程度的扰动时间内产生有用的预测。数据的模型可预测性随着​​我们移向更高的球谐度截断而增加,这是因为模型数据的失配减少了,但是由于合并了小规模特征而使粗糙度增加了。观测结果表明,球形谐波次数截断的增加与失配减少之间的这种关系可能受到数据质量或数量以及全局覆盖范围或分布的限制。

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