1997
DOI: 10.1029/97gl02055
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Energetic electron precipitation from the inner zone

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Cited by 12 publications
(7 citation statements)
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References 20 publications
(14 reference statements)
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“…Hess [] summarized the limited existing inner zone pre‐Starfish event results as showing that the “…spectrum is flat for 100 < Ee < 400 keV” and “… not certain whether there are any electrons present of E > 800 keV.” More recently, Abel et al . [, ] presented spectra of equatorially mirroring electrons for a few L values based on the CRRES Magnetic Electron Spectrometer A [ Vampola et al ., ] data. These showed relatively soft spectra for energies >500 keV and are discussed more below.…”
Section: Introductionmentioning
confidence: 99%
“…Hess [] summarized the limited existing inner zone pre‐Starfish event results as showing that the “…spectrum is flat for 100 < Ee < 400 keV” and “… not certain whether there are any electrons present of E > 800 keV.” More recently, Abel et al . [, ] presented spectra of equatorially mirroring electrons for a few L values based on the CRRES Magnetic Electron Spectrometer A [ Vampola et al ., ] data. These showed relatively soft spectra for energies >500 keV and are discussed more below.…”
Section: Introductionmentioning
confidence: 99%
“…[2] The coupling between the magnetosphere and the ionosphere through precipitating particles from radiation belts and the central plasma sheet that strongly controls ionization and conductance in the ionosphere has been known for some time, although it is one of the most difficult couplings to understand [e.g., Paulikas, 1975;Buonsanto, 1999;Ma et al, 2008;Kelley, 2009]. The energy deposition of precipitating particles of various energies mainly through the ionization of atmospheric atoms occurs at different altitudes, particularly within the D, E, and F regions of the ionosphere and extends from high to midlatitudes and over the South-Atlantic Anomaly (SAA) at low latitudes [e.g., Voss and Smith, 1980;Vampola and Gorney, 1983;Rees et al, 1988;Abel et al, 1997]. An impact of precipitating particles in the lower ionosphere (the D and E layers) and the upper atmosphere in terms of enhanced ionization and other related aeronomical effects has been investigated in a large number of studies [e.g., Buonsanto, 1999, and references therein;Nishino et al, 2002;Peter et al, 2006;Clilverd et al, 2008Clilverd et al, , 2010Turunen et al, 2009;Lam et al, 2010;Dmitriev et al, 2011], while evidence for ionospheric signatures in the topside ionosphere (F region) in the midlatitudes and over the SAA at low latitudes have also been reported [e.g., Foster et al, 1994Foster et al, , 1998Abdu et al, 2005;Kunitsyn et al, 2008aKunitsyn et al, , 2008bDmitriev and Yeh, 2008;Pedatella et al, 2009;Ngwira et al, 2012].…”
Section: Introductionmentioning
confidence: 99%
“…The very low likelihood of events potentially leading to direct injection or radial diffusion of relativistic electrons into the inner belt supports the conjecture of Kim and Shprits [2012] that any negative gradient in the phase space density of ≈ 0.5-1 MeV electrons toward higher L in the region L ∼ 1.5-2 [e.g., see Abel et al, 1997;Kim and Shprits, 2012;Fennell et al, 2015] would result either from very rare intrusions followed by very long periods (∼ year) dominated by losses to the atmosphere stronger at higher L in this region or from a local acceleration of lower energy (∼ 100 keV) electrons via resonant scattering by lightning-generated and VLF waves peaking near L = 1.5 − 1.7. However, energy diffusion by whistler-mode waves would require years to produce such a flux maximum .…”
Section: Discussionmentioning
confidence: 52%