THE STRUCTURE OF THE SOLAR WIND IN THE HELIOSPHERE DEPENDING ON THE PHASE OF THE SOLAR CYCLE: LARGE-SCALE DYNAMICS OF THE HELIOSPHERIC CURRENT SHEET

Authors

  • E. V. Maiewski Financial University under the Government of the Russian Federation; Space Research Institute (IKI), Russian Academy of Sciences
  • R. A. Kislov Space Research Institute (IKI), Russian Academy of Sciences; Heliophysical Laboratory, Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radiowave Propagation RAS (IZMIRAN)
  • H. V. Malova Space Research Institute (IKI), Russian Academy of Sciences; Lomonosov Moscow State University; Scobeltsyn Nuclear Physics Institute (NPI)
  • O. V. Khabarova Space Research Institute (IKI), Russian Academy of Sciences; Heliophysical Laboratory, Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radiowave Propagation RAS (IZMIRAN)
  • V. Yu. Popov Space Research Institute (IKI), Russian Academy of Sciences; National Research University “Higher School of Economics” Physics Department of Lomonosov Moscow State University
  • A. A. Petrukovich Space Research Institute (IKI), Russian Academy of Sciences
  • L. M. Zelenyi Space Research Institute (IKI), Russian Academy of Sciences

DOI:

https://doi.org/10.29006/1564-2291.JOR-2019.47(1).25

Keywords:

solar wind, solar magnetic field, heliospheric current system

Abstract

A stationary axisymmetric MHD model of the solar wind has been constructed, which allows us to study the spatial distribution of the magnetic field and plasma characteristics at radial distances from 20 to 400 radii of the Sun at almost all heliolatitudes. The model takes into account the changes in the magnetic field of the Sun during a quarter of the solar cycle, when the dominant dipole magnetic field is replaced by a quadrupole. Selfconsistent solutions for the magnetic and velocity fields, plasma concentration and current density of the solar wind depending on the phase of the solar cycle are obtained. It is shown that during the domination of the dipole magnetic component in the solar wind heliospheric current sheet (HCS) is located in the equatorial plane, which is a part of the system of radial and transverse currents, symmetrical in the northern and southern hemispheres. As the relative contribution of the quadrupole component to the total magnetic field increases, the shape of the HCS becomes conical; the angle of the cone gradually decreases, so that the current sheet moves entirely to one of the hemispheres. At the same time, at high latitudes of the opposite hemisphere, a second conical HCS arises, the angle of which increases. When the quadrupole field becomes dominant (at maximum solar activity), both HCS lie on conical surfaces inclined at an angle of 35 degrees to the equator. The model describes the transition from the fast solar wind at high latitudes to the slow solar wind at low latitudes: a relatively gentle transition in the period of low solar activity gives way to more drastic when high solar activity. The model also predicts an increase in the steepness of the profiles of the main characteristics of the solar wind with an increase in the radial distance from the Sun. Comparison of the obtained dependences with the available observational data is discussed.

Published

2019-05-29

Issue

Section

The XXII workshop of the Council of nonlinear dynamics of the Russian Academy of

Most read articles by the same author(s)