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[PEM10-P17] Comparison of Magnetic Variations Associated with the IHFAC Observed on the Ground and in the LEO
Keywords:IHFAC, LEO satellite, Geomagnetic Field Observation
Recently Ranasinghe et al.(2021) analyze a long term variation of the D-component magnetic variation at Davao (Geographical latitude 7 deg., Geographical longitude 124.5, Geomagnetic latitude -2.22 deg, Geomagnetic longitude 197.9 deg, Dip latitude -0.24 deg), and indicates that the direction of the IHFAC in the different local time shows the obvious seasonal variations. In particular, the obtained directions of IHFAC at the evening sector during September – November shows southward, which is inconsistent with the IHFAC model proposed by Fukushima (1979, 1991).
In this study, we analyze the data of Vector Field Magnetometer (VFM) onboard the Swam satellites to compare the characteristics of the IHFAC obtained from ground magnetometer data. The E-component (eastward) magnetic field variations in the NEC coordinate system from 2014 to 2021 is used in this study. We calculate the magnetic data obtained at a confined region of -5 < Lat < 5 (degree), and 115 < Long < 135 (degree) where Davao station is mostly centered.
As a result, the E-component magnetic field shows positive deviations in the dusk sectors from September to December, whereas it shows negative deviations from May to July. This signature is basically consistent with the observation on the ground by Ranasinghe et al. The result suggests the altitude of the IHFAC at equatorial region is higher than 510km of the altitude of Swam orbit. Moreover, this study implies the possibility to the more affordable observation in LEO by nano-satellites.