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- W1995651423 abstract "Magnetic ground data have previously been described, and a method for the quantitative determination of the equatorial electrojet parameters (by splitting up the regular daily variation SR into the electrojet component SRE and the planetary component SRP) presented (fambita-koye and Mayaud, 1975). Observed ‘apparent’ centres, obtained on this way, for the electrojet or the counter-electrojet, are here investigated. The actual action of various factors (asymmetry in the intensity of the total force on either side of the dip equator, shape of the dip equator on either side of the meridian of observation, asymmetry of the SRP(H) on either side of the centre or value of the SRP(z)) is pointed out. The ‘true’ centre, obtained by correcting observed values by the effect of these factors, is compared with the location of the dip equator, such as predicted by the POGO (8/69) model. For the electrojet, at mid-day hours, the ‘true’ centre coincides with that which we call the ‘efficient’ dip-equator (average location of it within a longitude sector of 30°). For the morning counter-electrojet, and, to a lesser extent, for the afternoon counter-electrojet events, the centre location is systematically about 40 km North. A tentative explanation of this deviation is given. Furthermore, one suggests that erratic locations of the centre in the early morning or in the late afternoon are due to large latitudinal gradients in the planetary SR vortices." @default.
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- W1995651423 date "1976-01-01" @default.
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- W1995651423 title "Equatorial electrojet and regular daily variation SR—II. the centre of the equatorial electrojet" @default.
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- W1995651423 doi "https://doi.org/10.1016/0021-9169(76)90189-6" @default.
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