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2017
DOI: 10.1007/s12517-017-3094-x
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The equatorial electrojet (EEJ) current deduced from CHAMP satellite and ground magnetic measurements in West Africa

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Cited by 2 publications
(2 citation statements)
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“…The present study focuses on the distribution and variability of Sq currents in the mid‐latitudes. However, the EEJ effects, which correspond to the structure of the eastward sheet currents show a V‐shaped depression near the geomagnetic equator, are located within a latitude band of about±12° on either side of the geomagnetic equator (Benaissa et al., 2017; Maus et al., 2007). To ensure the stability of the fitting algorithm for a more accurate simulation of the Sq current system, the geomagnetic eastward current in the geomagnetic latitude range between 12°S and 12°N is substituted with the fitted value obtained from a polynomial function of degree 12 calculated based on the current data from the mid‐latitude region.…”
Section: Methodsmentioning
confidence: 99%
“…The present study focuses on the distribution and variability of Sq currents in the mid‐latitudes. However, the EEJ effects, which correspond to the structure of the eastward sheet currents show a V‐shaped depression near the geomagnetic equator, are located within a latitude band of about±12° on either side of the geomagnetic equator (Benaissa et al., 2017; Maus et al., 2007). To ensure the stability of the fitting algorithm for a more accurate simulation of the Sq current system, the geomagnetic eastward current in the geomagnetic latitude range between 12°S and 12°N is substituted with the fitted value obtained from a polynomial function of degree 12 calculated based on the current data from the mid‐latitude region.…”
Section: Methodsmentioning
confidence: 99%
“…The EEJ current can be calculated using the idea that a pair of magnetometers, with one located at the dip magnetic equator (± 2°) and, while the other (an offequatorial station) should be located ± 6°-9° away from the magnetic equator, with both stations in the same longitudes as suggested by Rastogi & Klobuchar (1990), Anderson et al (2004), Yamazaki & Maute (2017). Following Tomás et al (2008), Benaissa et al (2017), due to the unavailability of The computed coordinates presented here are based on the Geomagnetic Coordinates IGRF-13 revised in December 2019 using the epoch of 2013 (data from British Geological Survey 2019).…”
Section: Methodsmentioning
confidence: 99%