Proton and electron heating by radially propagating fast magnetosonic waves
By R. Horne, G. Wheeler, H. Alleyne. 2000
181 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Geophysics
View Paper: https://www.semanticscholar.org/paper/bc0025aa3f866c6f3a2b9cc2fcdf0ed7bf35afc5
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Astronomy and Astrophysics
In Geophysics
Citations in the corpus
- Survey of magnetosonic waves and proton ring distributions in the Earth's inner magnetosphere (2008, background): “5 keV protons A number of theoretical studies have shown that magnetosonic waves can be generated 280 by a proton ring distribution in velocity space, or more specifically, a ring corresponding to 281 a positive gradient in the perpendicular velocity distribution of the protons which exceeds 282 the”
- Origins of plasmaspheric hiss (2006, background): “AttenuationintheEarth-ionospherewaveguideofa15.5kHz signal is expected to reduce the wave power by � 3 orders of magnitude over a distance of 1000 km [e.g., Helliwell, 1965, Figure 3.38].”
- Electron acceleration in the Van Allen radiation belts by fast magnetosonic waves (2007, background): “…waves are generated by a proton ring distribution at frequencies close to the harmonics of the proton gyrofrequency [Boardsen et al., 1992, Horne et al., 2000] and can propagate both inside and GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L17107, doi:10.1029/2007GL030267, 2007 1British…”
- The Electric and Magnetic Field Instrument Suite and Integrated Science (EMFISIS) on RBSP (2013, background): “The waves are observed both inside and outside the plasmapause and are excited by a cyclotron resonant instability with a ring distribution of injected ring current ions (Horne et al. 2000; Meredith et al. 2008; Chen et al. 2010b).”
- Radiation belt dynamics: The importance of wave‐particle interactions (2010, background): “The waves are observed both inside and outside the plasmapause and are excited by a cyclotron resonant instability with a ring distribution of injected ring current ions [Horne et al., 2000].”
- Transit time scattering of energetic electrons due to equatorially confined magnetosonic waves (2010, background): “These observations led early workers to the idea that MS waves derive their energy from a resonant interaction with a highly anisotropic “ring” distribution of energetic protons [e.g.,Gurnett, 1976; Perraut et al., 1982; Boardsen et al., 1992; Horne et al., 2000; Meredith et al., 2008].”
- Global simulation of magnetosonic wave instability in the storm time magnetosphere (2010, background): “When propagation characteristics are considered, the most unstable MS waves occur at a wave normal angle 89.5° [Horne et al., 2000, Figure 9].”
- Global simulation of EMIC wave excitation during the 21 April 2001 storm from coupled RCM‐RAM‐HOTRAY modeling (2010, background): “…ion distribution, which develops during transport and loss, should also be unstable to the excitation of equatorial magnetosonic waves [e.g., Boardsen et al., 1992,Horne et al., 2000] and the quasi‐linear scattering by such waves will also need to be incorporated into the evolving ion distribution.”
- Helium, Oxygen, Proton, and Electron (HOPE) Mass Spectrometer for the Radiation Belt Storm Probes Mission (2013, background): “Generally, five different wave modes can interact strongly with radiation belt electrons (Horne and Thorne 1998) including magnetosonic (Horne et al. 2000) and Z-mode waves (Glauert and Horne 2005).”