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The influence of nonmigrating tides on the longitudinal variation of the equatorial electrojet

机译:nonmigrating潮汐的影响赤道的纵向变化电喷流

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The climatological model of the equatorial electrojet, EEJM-1, derived from ?rsted, CHAMP and SAC-C satellite measurements provides the opportunity to investigate the longitudinal variation of the current strength in detail. Special emphasis is put in this study on the effect of nonmigrating tides. We have found that the influence of the diurnal eastward-propagating mode with wavenumber-3, DE3, is particularly strong. In polar orbiting satellite observations the DE3 tidal signal appears as a four-peaked longitudinal structure. We have put special emphasis in our analysis to isolate the DE3 contribution from other sources contributing to the wavenumber-4 structure in satellite data. The amplitude of the DE3 signature in the EEJ not only peaks during equinox seasons, but is also strong around the June solstice. When looking at the modulation of the EEJ intensity the DE3 accounts for about 25% during the months of April through September. It is thus the dominant cause for longitudinal variations. During December solstice months the influence of DE3 is negligible. A secondary three-peaked longitudinal pattern emerges during solstice seasons when the DE3 influence is removed. From the data available it is, however, not clear whether this pattern is related to any tidal drivers.
机译:赤道的气候模型电喷流、EEJM-1源自? rst,冠军和SAC-C卫星测量提供了纵向调查的机会电流强度的变化细节。特别重点放在这个研究nonmigrating潮汐的影响。周日eastward-propagating的影响模式与wavenumber-3 DE3,尤其强。作为一个four-peaked DE3潮汐信号出现纵向结构。在我们分析孤立DE3强调从其他来源造成的贡献在卫星数据wavenumber-4结构。振幅EEJ DE3签名的只有山峰在equinox的季节,但也是强大的夏至。DE3 EEJ强度的调制在4个月的约占25%到9月。纵向变化。冬至月DE3的影响可以忽略不计。模式时出现在冬至的季节DE3影响。然而,它是不清楚这种模式有关任何潮汐的司机。

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