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In the lower panels, the associated variations of the mean zonal mean electron density (in MHz) retrieved from COSMIC at 300 km during the two warmings are seen.
Because we mainly pay attention to the influence of DE3 tide on the ionospheric zonal mean states, we will mainly analyze the longitudinal and diurnal mean (zonal mean) states of ionosphere.
The lower boundary conditions are taken from the National Centres for Environmental Prediction and National Centre for Atmospheric Research reanalysis data, including monthly mean zonal mean temperature fields from 1,000 to 30 hPa as well as geopotential height and the corresponding amplitudes and phases of the first three stationary zonal harmonics at 1,000 hPa.
Thus, the influence of the background cannot be neglected and was removed by dividing the 8-h ES by the respective 3-monthly mean zonal mean ES OF. Figure 4 displays height-latitude cross sections of the normalised 8-h ES amplitude for solstice (DJF and JJA, left column) and equinox (MAM and SON, right column).
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Therefore, the 3-monthly mean zonal means from December 2006 to November 2012 were used for constructing a 6-year climatology.
Shown are 6-year averages, based on 3-monthly mean zonal means derived from FORMOSAT-3/COSMIC satellite measurements from December 2006 to November 2012.
The OF was sorted according to the local time (Figure 3, left panel), considering 3-monthly mean zonal means of an 11-km height interval.
Six-year averages based on the 3-monthly mean zonal means from December 2006 to November 2012 were constructed for the amplitude of the terdiurnal oscillation in the occurrence frequency of ES.
Shown are 3-monthly mean zonal means over an 11-km sliding height interval for solstice (December to February, left column) and equinox (March to May, right column), using the FORMOSAT-3/COSMIC satellite data from December 2006 to November 2012.
Shown are 3-monthly mean zonal means of October (September to November 20100, covering the latitudes from 43° to 63° N. As already described by Fytterer et al. (2013), the impact of DT and SDT has to be removed to validate the existence of the TDT.
The results show 3-monthly mean zonal means for winter (December to February, top left), spring (March to May, top right), summer (June to August, bottom left) and autumn (September to November, bottom right), derived from the FORMOSAT-3/COSMIC satellites measurements from December 2006 to November 2012.
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