THEMIS observations of long‐lived regions of large‐amplitude whistler waves in the inner magnetosphere
By Christopher Cully, John W. Bonnell, R. Ergun. 2008
146 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Geophysics
View Paper: https://www.semanticscholar.org/paper/e1bfe1594b8b1692c0048819bb5c4c5549a36a71
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Citations in the corpus
- Earth's Van Allen Radiation Belts: From Discovery to the Van Allen Probes Era (2019, background): “large‐amplitude chorus (e.g., Cattell et al., 2008; Cully et al., 2008; Kellogg et al., 2011; Tyler et al., 2019; Wilson et al., 2011), test particle simulations have demonstrated its general validity for small amplitude and broadband waves (Tao et al.”
- Global model of lower band and upper band chorus from multiple satellite observations (2012, methodology): “The high resolution (fff) data used here consists of measurements of one component of the magnetic wave spectral density in the spacecraft spin plane, with a frequency resolution with 32 or 64 frequency bands logarithmically spaced over 4–4000 Hz [Cully et al., 2008a].”
- Nonlinear interaction of energetic electrons with large amplitude chorus (2008, background): “[6] Here, we study the wave-particle interactions at L = 5 since this is the region where the largest amplitude chorus waves are present [Cully et al., 2008], maximum inferred internal acceleration occurs [Green and Kivelson, 2004],”
- Fine structure of large‐amplitude chorus wave packets (2014, background): “…Substorms, and Wind) have subsequently revealed that whistler mode waves with electric fields up to a few hundred mV/m can exist in the inner magnetosphere [Cattell et al., 2008; Cully et al., 2008; Kellogg et al., 2011] although their properties sometimes show distinct differences from chorus.”
- Resonant scattering of plasma sheet electrons leading to diffuse auroral precipitation: 2. Evaluation for whistler mode chorus waves (2011, background): “However, in a recent statistical study using the THEMIS filter bank wave data, Li et al. [2009a] found that nightside chorus waves tend to maximize at L < 7 and become weak or disappear at L > ∼8.”
- The Electric Field Instrument (EFI) for THEMIS (2008, methodology): “Note that while the short axial booms do lead to significant issues with the DC field measurement, the AC field mea- surement (above a few hundred Hz) does not suffer from these failings, and has been used to make clean, three-dimensional E-field estimates successfully (e.g. Cully et al. 2008a).”
- Global distribution of whistler‐mode chorus waves observed on the THEMIS spacecraft (2009, methodology): “The resulting wave amplitudes (filter bank data) are included in the survey mode telemetry, covering most orbits with a measurement cadence of four seconds [Cully et al., 2008a].”
- Statistics of whistler mode waves in the outer radiation belt: Cluster STAFF‐SA measurements (2013, background): “The obtained spatial distributions are consistent with the earlier plasmaspheric hiss observations aboard DE-1 [André et al., 2002; Green et al., 2005] and aboard CRRES [Meredith et al., 2004], and lower band chorus statistics from CRRES [Meredith et al., 2001], THEMIS [Cully et al., 2008; Li et al.”
- Radiation belt dynamics: The importance of wave‐particle interactions (2010, unknown): “%) of occurrence [Cully et al., 2008].”