2015
DOI: 10.1002/2015rs005711
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Power spectrum analysis of ionospheric fluctuations with the Murchison Widefield Array

Abstract: Low-frequency, wide field-of-view (FOV) radio telescopes such as the Murchison Widefield Array (MWA) enable the ionosphere to be sampled at high spatial completeness. We present the results of the first power spectrum analysis of ionospheric fluctuations in MWA data, where we examined the position offsets of radio sources appearing in two data sets. The refractive shifts in the positions of celestial sources are proportional to spatial gradients in the electron column density transverse to the line of sight. T… Show more

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Cited by 38 publications
(60 citation statements)
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References 88 publications
(138 reference statements)
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“…In each snapshot image, the ionosphere introduces a random displacement (typically 10-20 arcsec) in the source positions (Loi et al 2015). This smears out sources in the mosaicked image.…”
Section: Discussion and Future Workmentioning
confidence: 99%
“…In each snapshot image, the ionosphere introduces a random displacement (typically 10-20 arcsec) in the source positions (Loi et al 2015). This smears out sources in the mosaicked image.…”
Section: Discussion and Future Workmentioning
confidence: 99%
“…Most of our knowledge of the large‐scale ionosphere is derived from measurements from dedicated experiments with ionosondes and GPS satellites and receivers. Measurements of ionospheric structure have been done by radio telescopes before, for example, traveling ionospheric disturbances (TIDs) [ van Velthoven , ; Spoelstra , ; Helmboldt et al , ], turbulent like fluctuations [ Spoelstra , ; Cohen and Röttgering , ] and plasmaspheric irregularities [ Jacobson and Erickson , ; Helmboldt et al , ; Loi et al , ]. LOFAR can contribute to these measurements in a unique way.…”
Section: Introductionmentioning
confidence: 98%
“…Animations of the distortion vector field for each of the three nights are shown in Movies S1, S2, and S3 in the supporting information (see Loi et al [] for an explanation of the visualization scheme). In all plots, black solid lines are the geomagnetic field lines from L = 1.8, computed assuming a simple dipole model with the MWA at a geomagnetic latitude of 38.6°S and a magnetic declination of 0° (this is more accurately −0.153° [ Thébault et al , ], but we neglect this for simplicity of plotting).…”
Section: Resultsmentioning
confidence: 99%
“…These were obtained by taking the Fourier transform of the data cubes with all measurement values replaced by unity. Details of the method can be found in Loi et al [2015b]. The negative slope of the ringing features in the response functions arise from the drift of celestial sources as the Earth rotates, which produces diagonal tracks in the spatiotemporal sampling pattern.…”
Section: Appendix B: Power Spectrum Response Functionsmentioning
confidence: 99%
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