The Disturbance storm time (Dst) index has been widely used as a proxy for the ring current intensity, and therefore as a measure of geomagnetic activity. It is derived by measurements from four ground magnetometers in the geomagnetic equatorial regions. We present a new model for predicting $Dst$ with a lead time between 1 and 6 hours. The model is first developed using a Gated Recurrent Unit (GRU) network that is trained using solar wind parameters. The uncertainty of the $Dst$ model is then estimated by using the ACCRUE method [Camporeale et al. 2021]. Finally, a multi-fidelity boosting method is developed in order to enhance the accuracy of the model and reduce its associated uncertainty. It is shown that the developed model can predict $Dst$ 6 hours ahead with a root-mean-square-error (RMSE) of 13.54 $\mathrm{nT}$. This is significantly better than the persistence model and a simple GRU model.
翻译:扰动风暴时间指数(Dst)已被广泛用作环形当前强度的替代物,因此是地磁活动的一种测量尺度。它来自地磁赤道地区四个地面磁强计的测量结果。我们提出了一个新的模型来预测1至6小时的周转时间$Dst;该模型最初是使用利用太阳能风参数培训的Gate 经常单元(GRU)网络开发的。然后通过使用ACCRUE方法[Camporeale 等2021]来估计美元模型的不确定性。最后,开发了一种多纤维增强法,以提高模型的准确性并减少其相关的不确定性。显示,开发的模型可以提前6小时预测$Dstt$,而根-平均值-方格-error(RMSE)为13.54美元/mathrm{nT}。这比持久性模型和一个简单的GRU模型要好得多。