Abstract

Models based on neural networks and machine learning are seeing a rise in popularity in space physics. In particular, the forecasting of geomagnetic indices with neural network models is becoming a popular field of study. These models are evaluated with metrics such as the root-mean-square error (RMSE) and Pearson correlation coefficient. However, these classical metrics sometimes fail to capture crucial behavior. To show where the classical metrics are lacking, we trained a neural network, using a long short-term memory network, to make a forecast of the disturbance storm time index at origin time $t$ with a forecasting horizon of 1 up to 6 hours, trained on OMNIWeb data. Inspection of the model's results with the correlation coefficient and RMSE indicated a performance comparable to the latest publications. However, visual inspection showed that the predictions made by the neural network were behaving similarly to the persistence model. In this work, a new method is proposed to measure whether two time series are shifted in time with respect to each other, such as the persistence model output versus the observation. The new measure, based on Dynamical Time Warping, is capable of identifying results made by the persistence model and shows promising results in confirming the visual observations of the neural network's output. Finally, different methodologies for training the neural network are explored in order to remove the persistence behavior from the results.

Highlights

  • The disturbance storm time (Dst) index is calculated from the measurements of four ground-based magnetometer stations, located close to the equator and spread evenly across the Earth (Sugiura and Kamei, 1991)

  • The linear relation of the persistence model is consistently better for every forecasting horizon compared to the long short-term memory (LSTM)-NN model

  • We find that for both root-mean-square error (RMSE) and correlation, the reported performance of the LSTM-NN and the persistence model lies inside the variation, indicating that there is no artificial improvement of the results by choosing an ideal training and test set

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Summary

Introduction

The disturbance storm time (Dst) index is calculated from the measurements of four ground-based magnetometer stations, located close to the equator and spread evenly across the Earth (Sugiura and Kamei, 1991). The index, introduced by Sugiura (1963), is the average of the magnetic disturbance of the Earth’s magnetic field horizontal component. Geomagnetic storms are large perturbations in the Earth’s magnetic field. They are caused by the coupling between solar wind and magnetosphere, in particular the southward component of the interplanetary magnetic field (IMF) (Burton et al, 1975). When magnetic reconnection happens between the IMF and the Earth’s magnetosphere, an influx of energetic particles from the solar wind into the magnetosphere occurs. This increases the intensity of the Earth’s ring

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