Quantification of Energetic Electron Precipitation Driven by Plume Whistler Mode Waves, Plasmaspheric Hiss, and Exohiss

Quantification of Energetic Electron Precipitation Driven by Plume Whistler Mode Waves, Plasmaspheric Hiss, and Exohiss
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DOI:
10.1029/2019gl082095
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发表时间:
2019-04
影响因子:
5.2
通讯作者:
W. Li;X. Shen;Q. Ma;L. Capannolo;R. Shi;R. Redmon;J. Rodriguez;G. Reeves;C. Kletzing;W. Kurth;G. Hospodarsky
W. Li;X. Shen;Q. Ma;L. Capannolo;R. Shi;R. Redmon;J. Rodriguez;G. Reeves;C. Kletzing;W. Kurth;G. Hospodarsky
中科院分区:
地球科学1区
文献类型:
--
作者:
W. Li;X. Shen;Q. Ma;L. Capannolo;R. Shi;R. Redmon;J. Rodriguez;G. Reeves;C. Kletzing;W. Kurth;G. Hospodarsky

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Whistler mode waves are important for precipitating energetic electrons into Earth's upper atmosphere, while the quantitative effect of each type of whistler mode wave on electron precipitation is not well understood. In this letter, we evaluate energetic electron precipitation driven by three types of whistler mode waves: plume whistler mode waves, plasmaspheric hiss, and exohiss observed outside the plasmapause. By quantitatively analyzing three conjunction events between Van Allen Probes and POES/MetOp satellites, together with quasi‐linear calculation, we found that plume whistler mode waves are most effective in pitch angle scattering loss, particularly for the electrons from tens to hundreds of keV. Our new finding provides the first direct evidence of effective pitch angle scattering driven by plume whistler mode waves and is critical for understanding energetic electron loss process in the inner magnetosphere. We suggest the effect of plume whistler mode waves be accurately incorporated into future radiation belt modeling.