2014
DOI: 10.1002/2014ja020406
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Broadband meter‐wavelength observations of ionospheric scintillation

Abstract: Intensity scintillations of cosmic radio sources are used to study astrophysical plasmas like the ionosphere, the solar wind, and the interstellar medium. Normally, these observations are relatively narrow band. With Low‐Frequency Array (LOFAR) technology at the Kilpisjärvi Atmospheric Imaging Receiver Array (KAIRA) station in northern Finland we have observed scintillations over a three‐octave bandwidth. “Parabolic arcs,” which were discovered in interstellar scintillations of pulsars, can provide precise est… Show more

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Cited by 25 publications
(29 citation statements)
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“…Ionospheric scintillation affects sources with angular sizes 10 ( Loi et al 2015b) and the latter usually not very significant (although see Fallows et al 2014). Therefore, ionospheric refraction should affect the thousands of unresolved sources in each image.…”
Section: Origin Of Variabilitymentioning
confidence: 99%
“…Ionospheric scintillation affects sources with angular sizes 10 ( Loi et al 2015b) and the latter usually not very significant (although see Fallows et al 2014). Therefore, ionospheric refraction should affect the thousands of unresolved sources in each image.…”
Section: Origin Of Variabilitymentioning
confidence: 99%
“…The Kilpisjärvi Atmospheric Imaging Receiver Array (KAIRA; McKay-Bukowski et al (2014)), a station built using LOFAR hardware in arctic Finland, has been routinely monitoring the ionosphere, including ionospheric scintillation, since 2012 (e.g. Fallows et al 2014): The ionospheric scintillation conditions above KAIRA are naturally more severe than above LOFAR: At auroral latitudes, refractive index gradients due to fieldline elongated ionisation structures are stronger than in the case of middle latitudes structures. These observations can, therefore, be used to verify the effects of periods of strong ionospheric scintillation.…”
Section: Introductionmentioning
confidence: 99%
“…The first stage of analysis was the calculation of delay-Doppler spectra: these were created from the dynamic spectra using 5-min time slices, advancing every minute through the observation, following the methods described in Fallows et al (2014). To avoid regions more heavily contaminated by RFI, the frequency band used was restricted to 28.5-64.1 MHz.…”
Section: Delay-doppler Spectramentioning
confidence: 99%
“…The presence of two scintillation arcs likely indicates that scattering is dominated by two distinct layers in the ionosphere. A simple analysis, as described in Fallows et al (2014), can be used to estimate the altitude of the scattering region with a basic formula relating arc curvature C to velocity V and distance L along the line of sight to the scattering region (Cordes et al, 2006): The square term for the velocity illustrates the importance of gaining a good estimate of velocity to be able to accurately estimate the altitude of the scattering region via this method.…”
Section: Delay-doppler Spectramentioning
confidence: 99%
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