2008
DOI: 10.1029/2008ja013039
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Conditional integration of Incoherent Scattering in relation to flickering aurora

Abstract: [1] In this report we present incoherent scatter radar (ISR) observations of ionospheric response to precipitation causing flickering aurora. Flickering aurora is caused by electron precipitation with modulations at frequencies higher than 5 Hz. To resolve the variation at these short time-scales with ISR we have integrated together pulses at the same phase of the optical intensity variation observed with high-speed narrow field-of-view imaging in white light to determine the intensity variation in the field a… Show more

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Cited by 6 publications
(7 citation statements)
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“…Although EISCAT data will primarily show the result of the continuous nonflickering precipitation, we would expect to see more enhancement at higher altitudes if the flickering had a significant low‐energy component. Grydeland et al [2008] showed that flickering precipitation can modulate the radar backscattered power from the upper E region. Their EISCAT experiment did not record backscatter from below 130 km, so it is not known whether there were larger modulations in the lower E region.…”
Section: Resultsmentioning
confidence: 99%
“…Although EISCAT data will primarily show the result of the continuous nonflickering precipitation, we would expect to see more enhancement at higher altitudes if the flickering had a significant low‐energy component. Grydeland et al [2008] showed that flickering precipitation can modulate the radar backscattered power from the upper E region. Their EISCAT experiment did not record backscatter from below 130 km, so it is not known whether there were larger modulations in the lower E region.…”
Section: Resultsmentioning
confidence: 99%
“…When such temporally varying precipitation enters the ionosphere, it causes excitation and ionization with different temporal response at different altitudes [ Peticolas and Lummerzheim , 2000]. In addition to temporal variation in ionization the modulated electron precipitation also leads to temporal variation electron heating, the effect of this have been observed to be a 100 K modulation of the electron temperature [ Grydeland et al , 2008].…”
Section: Introductionmentioning
confidence: 99%
“…These two main frequency ranges correspond broadly to the ion cyclotron frequencies of O + and H + at 1 R E (≈10 Hz and ≈100 Hz respectively). In most known cases only a small proportion of the total aurora intensity is flickering, typically 10–20 percent [ Kunitake and Oguti , 1984; Sakanoi and Fukunishi , 2004; Grydeland et al , 2008]. Previous reports of flickering aurora have almost exclusively concentrated on patches with scale sizes larger than 1 km.…”
Section: Introductionmentioning
confidence: 99%