4.7 Article

Characteristics of hiss-like and discrete whistler-mode emissions

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 39, Issue -, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2012GL053206

Keywords

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Funding

  1. NASA [NNX11AD75G, NNX11AR64G, NNX08AI35G, NAS5-02099]
  2. NSF grant [AGS-0840178]
  3. German Ministry for Economy and Technology
  4. German Center for Aviation and Space (DLR) [50 OC 0302]
  5. NASA [100787, NNX08AI35G] Funding Source: Federal RePORTER
  6. Directorate For Geosciences [0903802] Funding Source: National Science Foundation
  7. Div Atmospheric & Geospace Sciences [0903802] Funding Source: National Science Foundation

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The characteristics of hiss-like and discrete (rising and falling tones) whistler-mode waves in the lower-band wave frequency range (0.1-0.5 of equatorial electron gyrofrequency) are investigated using waveform data from near-equatorially orbiting multiple THEMIS spacecraft outside the plasmasphere. Statistical results show that wave polarization properties of hiss-like emissions are similar to rising tones, but are significantly different from falling tones. The magnetic wave amplitudes of hiss-like bands and rising tones are generally larger than those of falling tones. Wave normal angles of broadband hiss-like emissions and rising tones tend to be quasi field-aligned, whereas falling tones are very oblique. Importantly, discrete emissions including rising and falling tones are predominantly observed in the region of low f(pe)/f(ce) (the ratio of plasma frequency to electron gyrofrequency), whereas hiss-like bands alone preferentially occur in the region of high f(pe)/f(ce). These important features of hiss-like and discrete whistler-mode emissions should be considered when evaluating their interactions with energetic electrons. Citation: Li, W., R. M. Thorne, J. Bortnik, X. Tao, and V. Angelopoulos (2012), Characteristics of hiss-like and discrete whistler-mode emissions, Geophys. Res. Lett., 39, L18106, doi: 10.1029/2012GL053206.

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