Abstract

Analysis of 163 isolated substorms showed that their intensity quantified as a maximum absolute value of the AL index increases with an increase in the velocity and number density of the solar wind plasma and hence its dynamic pressure. Most of the coupling functions describing the energy loading to the magnetosphere, e.g., the Kan–Lee electric field (EKL) and the Newell factor (dΦ/dt), do not include the dynamic pressure as an input parameter. Having examined the correlation between these functions and the dynamic pressure, we found that, surprisingly, while almost uncorrelated for any arbitrary time interval, both EKL and dΦ/dt correlate with the dynamic pressure within 1 h before the onset of isolated substorms. That is, an increase in the solar wind dynamic pressure is associated with an increase in the solar wind driving before the onset. We assume that the increase in the dynamic pressure as early as before substorm growth path creates the conditions inside the magnetosphere that impede the occurrence of substorms and increase the threshold for the instability leading to expansion onset, forcing the accumulation of greater amount of energy in the magnetosphere. This energy is released during substorm expansion, producing a more intense magnetic bay.

Highlights

  • The concept of classical substorm is based on the loading of solar wind energy into the Earth’s magnetosphere followed by a sudden release of this energy during substorm expansion

  • We test the hypothesis that prior to the substorm growth phase the solar wind plasma parameters determine the magnetospheric state, and to a large extent determine the intensity of a following isolated substorm

  • We study the behavior of the interplanetary magnetic field (IMF) components, as well as of the solar wind velocity, number density, and dynamic pressure, preceding isolated substorms of different intensities, in order to examine their influence on the energy loading to the magnetosphere before substorm onset

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Summary

Introduction

The concept of classical substorm is based on the loading of solar wind energy into the Earth’s magnetosphere followed by a sudden release of this energy during substorm expansion. Vorobjev et al (2016) made a statistical study of the loading–unloading processes of the magnetosphere during isolated substorms and showed that there is a strong relationship between the integral values of energy uploaded to the magnetosphere during the growth and expansive phases and the substorm intensity quantified as a total energy of auroral precipitation.

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