Abstract

Abstract Low-frequency (quasi-)monochromatic electromagnetic waves near the ion-cyclotron frequency always exhibit both left-hand (LH) and right-hand (RH) polarization in solar-terrestrial spacecraft observations. However, due to the Doppler frequency shift resulting from the bulk flow of charged particles, the nature of these waves in the plasma frame is still unclear. This paper proposes a useful method to directly identify the nature of the observed waves. Using three wave parameters including polarization, direction of the parallel Poynting flux, and correlation between perpendicular magnetic field and perpendicular ion/electron velocity, we could discriminate the wave mode (Alfvén/ion-cyclotron wave or fast-magnetosonic/whistler wave) and its propagation direction (along or against the magnetic field) in the plasma frame. Using Magnetospheric Multiscale spacecraft measurements, we analyze two wave events containing both LH- and RH-polarized low-frequency electromagnetic waves in the Earth’s magnetosheath, and find that these waves correspond to counter-propagating Alfvén/ion-cyclotron waves in the plasma frame. Our method is helpful for studying low-frequency electromagnetic waves detected by satellites that have particle measurements with an adequate temporal resolution.

Highlights

  • The Alfvén/ion-cyclotron wave is a left-hand (LH) polarized wave in a motionless plasma, and this mode is specially named the electromagnetic ion-cyclotron wave as the wave frequency ω approximates the ion-cyclotron frequency ωci

  • Different from the Alfvén/ioncyclotron wave limited by ω < ωci, the fast-magnetosonic/ whistler wave can extend to frequencies larger than ωci in the plasma frame (Huang et al 2019)

  • Dispersion relation; polarization defined as B0)-1; the ratio of electron velocity to magnetic field fluctuation (Ve^ VA)(B^ B0)-1; and the parallel Poynting flux normalized by 2VA WB the waves propagating along and against the magnetic field, respectively

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Summary

Introduction

The Alfvén/ion-cyclotron wave is a left-hand (LH) polarized wave in a motionless plasma, and this mode is specially named the electromagnetic ion-cyclotron wave as the wave frequency ω approximates the ion-cyclotron frequency ωci. The cyclotron resonant interaction of electromagnetic ion-cyclotron waves with ions can contribute to the acceleration of the fast solar wind (e.g., Cranmer 2001; Hollweg & Isenberg 2002; Ofman et al 2002) Another low-frequency electromagnetic wave mode is the right-hand (RH) polarized fast-magnetosonic/whistler wave (Gary 1993; Huang et al 2019). When the charged particles have a bulk flow propagating along the ambient magnetic field at a velocity larger than the wave phase speed, the observed LH-polarized electromagnetic wave can be the forward (along the magnetic field) Alfvén/ion-cyclotron wave or the backward (against the magnetic field) fast-magnetosonic/whistler wave in the plasma frame (Gary et al 2016). The observed RH-polarized electromagnetic wave can be the forward fast-magnetosonic/ whistler wave or the backward Alfvén/ion-cyclotron wave in the plasma frame (Gary et al 2016). This paper presents two applications on analyses of the observed LH- and RH-polarized electromagnetic waves in Section 3, illustrating the validation of our method

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