Abstract
We present the first statistical analysis with continuous data coverage and nonaveraged amplitudes of the prevalence and distribution of high-amplitude (>5 mV/m) whistler mode waves in the outer radiation belt using 5 years of Van Allen Probes data. These waves are most common above L = 3.5 and between magnetic local time of 0–7 where they are present 1–4% of the time. During high geomagnetic activity, high-amplitude whistler mode wave occurrence rises above 30% in some regions. During these active times the plasmasphere erodes to lower L and high-amplitude waves are observed at all L outside of it, with the highest occurrence at low L (3.5–4) in the predawn sector. These results have important implications for modeling radiation belt particle interactions with chorus, as large-amplitude waves interact nonlinearly with electrons. Results also may provide clues regarding the mechanisms which result in growth to large amplitudes.
Original language | English (US) |
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Pages (from-to) | 2328-2336 |
Number of pages | 9 |
Journal | Geophysical Research Letters |
Volume | 46 |
Issue number | 5 |
DOIs | |
State | Published - Mar 16 2019 |
Bibliographical note
Publisher Copyright:©2019. American Geophysical Union. All Rights Reserved.
Keywords
- Van Allen belt
- chorus
- radiation belt
- whistler waves