Global model of lower band and upper band chorus from multiple satellite observations
By Nigel P. Meredith, R. Horne, A. Sicard-Piet, D. Boscher, K. Yearby, Wen Li, R. Thorne. 2012
253 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Geophysics
View Paper: https://www.semanticscholar.org/paper/c1ec810921c904e71585ac66f26605fdddbcdeaf
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Citations in the corpus
- Particle Dynamics in the Earth's Radiation Belts: Review of Current Research and Open Questions (2020, background): “…polarized whistler mode waves that are observed in two distinct frequency bands outside the plasmasphere up to geostationary orbits and beyond (e.g., Allcock, 1957; Bunch et al., 2013; LeDocq et al., 1998; Meredith et al., 2012; Meredith, Horne, Li, et al., 2014; Tsurutani & Smith, 1974).”
- Radiation belt electron acceleration by chorus waves during the 17 March 2013 storm (2014, background): “The latitudinal extent (|λ|) of chorus waves varies in different MLT sectors based on the statistical results [Meredith et al., 2012; Agapitov et al., 2013].”
- Three‐dimensional electron radiation belt simulations using the BAS Radiation Belt Model with new diffusion models for chorus, plasmaspheric hiss, and lightning‐generated whistlers (2014, background): “Electrons trapped in the Earth’s radiation belts encounter several different types of electromagnetic waves as they drift around the Earth, including whistler mode chorus, plasmaspheric hiss, and LGW.”
- Electron losses from the radiation belts caused by EMIC waves (2014, background): “Chorus waves tend to be most significant outside the plasmapause on the dawnside during active conditions [Meredith et al., 2001, 2012; Li et al., 2011].”
- Earth's Van Allen Radiation Belts: From Discovery to the Van Allen Probes Era (2019, methodology): “Before the Van Allen Probes era, empirical chorus wave distributions based on satellite wave measurements (Agapitov et al., 2013, 2018; Li et al., 2011, 2009; Meredith et al., 2012; Meredith, Horne, et al., 2003) were used to calculate diffusion coefficients driven by chorus waves.”
- Evolution and slow decay of an unusual narrow ring of relativistic electrons near L ~ 3.2 following the September 2012 magnetic storm (2013, background): “both chorus emissions, which are generated in the low density region outside the plasmapause [Meredith et al., 2012], and hiss, which is confined inside the plasmapause [Meredith et al.”
- Statistics of whistler mode waves in the outer radiation belt: Cluster STAFF‐SA measurements (2013, methodology): “Occurrence rate is quite close to the observed by THEMIS spacecraft in the equatorial region [Cully et al., 2008; Li et al., 2011; Meredith et al., 2012].”
- Global morphology and spectral properties of EMIC waves derived from CRRES observations (2014, methodology): “For our chorus wave database [Meredith et al., 2012] we initially averaged the wave data as a function of L∗ and half orbit in steps of 0.1L∗.”
- Constructing the global distribution of chorus wave intensity using measurements of electrons by the POES satellites and waves by the Van Allen Probes (2013, methodology): “We assume a typical chorus wave frequency spectrum and wave normal distributions based on statistical results [Meredith et al., 2012; Li et al., 2011, 2013].”
- Statistical properties of plasmaspheric hiss derived from Van Allen Probes data and their effects on radiation belt electron dynamics (2015, background): “…chorus waves typically observed in the plasmatrough region with frequencies between 0.1 and 0.8 fce, where fce is the electron cyclotron frequency [e.g., Burtis and Helliwell, 1969; Burton and Holzer, 1974; Tsurutani and Smith, 1974, 1977; Meredith et al., 2003, 2012; Li et al., 2009, 2011].”
- Energetic electron precipitation associated with pulsating aurora: EISCAT and Van Allen Probe observations (2015, methodology): “Furthermore, it is assumed that LBC propagates to the magnetic latitude of 20°, based on the statistical analysis [Meredith et al., 2012].”