Abstract

Abstract. The spatial distribution and source-region size of chorus waves are important parameters for understanding their generation. In this work, we analyze over 3 years of continuous wave burst-mode data from the Van Allen Probes mission and build a data set of rising-tone and falling-tone chorus waves. For the L shell range covered by Van Allen Probes data (3.5≤L≤7), statistical results demonstrate that the sector where rising tones are most likely to be observed is the dayside during geomagnetically quiet and moderate times and the dawn side during active times. Moreover, rising-tone chorus waves have a higher occurrence rate near the equatorial plane, while the falling-tone chorus waves have a higher possibility to be observed at lower L shell and higher magnetic latitudes. By analyzing the direction of the Poynting wave vector, we statistically investigate the chorus source-region size along a field line, and compare the results with previous theoretical estimates. Our analysis confirms previous conclusions that both rising-tone and falling-tone chorus waves are generated near the equatorial plane, and shows that previous theoretical estimates roughly agree with the observation within a factor of 2. Our results provide important insights into further understanding of chorus generation.

Highlights

  • Chorus waves are whistler mode waves consisting of discrete coherent elements with frequency chirping

  • Our analysis shows that the spatial distribution of the occurrence rate of rising and falling-tone chorus during periods of different geomagnetic activities is different

  • Rising-tone chorus waves mainly occur at the dayside sector during quiet times and move to dawn side during active conditions

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Summary

Introduction

Chorus waves are whistler mode waves consisting of discrete coherent elements with frequency chirping. Using Van Allen Probes wave observations, Li et al (2016) found that quasi-parallel chorus waves dominate over quasielectrostatic ones during more disturbed geomagnetic periods and at higher L shells They did not differentiate between rising or falling tones in the statistical results, since they used the survey mode wave data from the Van Allen Probes, which has low time resolution (1 sample per 6 s), while the frequency of discrete elements of chorus changes on the order of 1 kHz typically within less than a second. We use high-resolution burst-mode waveform data with a sampling rate of 35 kHz from Van Allen Probes to analyze the spatial distribution of the rising-tone and falling-tone chorus under different geomagnetic activity conditions.

Data base and event selection
Spatial distribution of rising-tone and falling-tone chorus
The source-region size of chorus
Observation
Comparison between the theoretical source-region size and observation
Findings
Summary
Full Text
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