Abstract

We present the results of an effort to model quiet-time vertical plasma drifts in the low-latitude F-region ionosphere using the random forest machine learning technique. The model is capable of describing the climatological variation of the drifts as a function of universal time, day of the year, solar flux, and altitude (200–600 km). The model has been trained using measurements of the vertical plasma drifts made by the incoherent scatter radar of the Jicamarca Radio Observatory (11.95^circ hbox { S}, 76.87^circ W, sim 1^circ dip lat). In our analysis, we compare our machine learning model results with the Scherliess and Fejer (J Geophys Res 104:6829–6842, 1999) model (SF99 model), a widely used empirical model of the vertical drifts developed using a different set of Jicamarca measurements. We find that the machine learning model is able to capture the overall features of the diurnal variation of the equatorial drifts for different seasonal and solar flux conditions. The model is also capable of capturing the mean height variation of the drifts, particularly the height gradient enhancements that have been observed near sunrise and sunset. Finally, the model can easily be expanded and improved as more drift measurements are made and become available for training.

Highlights

  • The zonal component of the ionospheric electric field in the magnetic equatorial region plays an important role in the dynamics of the geospace environment with implications for space weather

  • We present the results of an effort to model quiet-time vertical plasma drifts in the low-latitude F-region ionosphere using the random forest machine learning technique

  • We compare our machine learning model results with the Scherliess and Fejer (1999) model (SF99 model), a widely used empirical model of the vertical drifts developed using a different set of Jicamarca measurements

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Summary

Introduction

The zonal component of the ionospheric electric field in the magnetic equatorial region plays an important role in the dynamics of the geospace environment with implications for space weather. This electric field is one of the main drivers of ionospheric plasma transport at low- and mid-latitude regions (e.g., Klobuchar et al 1991). Pressure and gravitational forces will cause the plasma to diffuse poleward along magnetic field lines This “fountain” effect results in ionization peaks at higher magnetic latitudes, a phenomenon referred to as the equatorial ionization anomaly (EIA) or Appleton anomaly (Schunk and Nagy 2009)

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