2020
DOI: 10.1016/j.jastp.2020.105400
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Detecting ionospheric disturbances using GPS without aliasing caused by non-uniform spatial sampling: Algorithm, validation and illustration

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“…Figure 3 illustrates the keograms of the filtered TECs of New Zealand and Australia (Figures 3a and 3c) and Japan (Figures 3b and 3d). It is noteworthy that only TEC observations with elevation angle >30° are utilized to mitigate the effect from the non‐uniform spatial interval of ionospheric‐pierce‐points (Shimna & Vijayan, 2020). As the filtered TECs over Japan are mapped to the southern hemisphere, the distances to the volcano are counted from their southern hemisphere magnetic conjugate locations.…”
Section: Gnss Tec Observationsmentioning
confidence: 99%
“…Figure 3 illustrates the keograms of the filtered TECs of New Zealand and Australia (Figures 3a and 3c) and Japan (Figures 3b and 3d). It is noteworthy that only TEC observations with elevation angle >30° are utilized to mitigate the effect from the non‐uniform spatial interval of ionospheric‐pierce‐points (Shimna & Vijayan, 2020). As the filtered TECs over Japan are mapped to the southern hemisphere, the distances to the volcano are counted from their southern hemisphere magnetic conjugate locations.…”
Section: Gnss Tec Observationsmentioning
confidence: 99%