Abstract

It has been known that the Alfvén velocity plays a significant role in generation and propagation of magnetohydrodynamic (MHD) waves. Until now, however, the global distribution of the Alfvén velocity in the magnetosphere has not been reported. To determine the spatial distribution of the Alfvén velocity, we have statistically examined the THEMIS magnetic field and electron density data obtained in the L (the equatorial geocentric distance to the field line measured in Earth’s radii) range of ~ 4–12 and at all local times near the magnetic equator between − 5° and 5° in magnetic latitude for 2008–2014. We observed a pronounced dawn–dusk asymmetry in the equatorial Alfvén velocity calculated from the THEMIS magnetic field and density data. That is, the dawnside Alfvén velocity is higher than the duskside Alfvén velocity. This asymmetry is due to the duskside bulge in the plasmasphere. The radial profile of the Alfvén velocity shows an increasing function of L between L = 4 and 10 in the dusk sector, while a decreasing function in the dawn sector. By comparing these Alfvén velocity distributions along the local time and radial distance, we discuss the occurrence distribution and propagation of MHD waves in the outer magnetosphere.

Highlights

  • Magnetohydrodynamic (MHD) waves have become recognized as a manifestation of energy transport in the Earth’s magnetosphere and serve as a useful tool for remote sensing of the magnetospheric phenomena

  • THEMIS-A was near the magnetic equator with a magnetic latitude (MLAT) between − 1.7° and 4.4°, and it moved outward from L = 3.2 in the morning (MLT = 9.2) to L = 11.3 in the afternoon (MLT = 13.1)

  • By using the magnetic field and electron density observed in the L range of ~ 4–12 and at all local times near the magnetic equator, we obtain the spatial distribution of equatorial VA

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Summary

Introduction

Magnetohydrodynamic (MHD) waves have become recognized as a manifestation of energy transport in the Earth’s magnetosphere and serve as a useful tool for remote sensing of the magnetospheric phenomena. The MHD wave equations produce three wave modes: the shear Alfvén mode, slow mode, and fast mode. The wave packet for the shear Alfvén mode propagates only along the ambient magnetic field, while the fast mode propagates isotropically and delivers wave energy across the field lines. The fast mode speed is similar to the Alfvén velocity except for a region of the plasma sheet, where the plasma temperature is very high (Moore et al 1987). The Alfvén velocity is determined from magnetospheric fundamental quantities, plasma mass density, and magnetic field intensity.

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