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They observed the counter-Sq SFE in limited longitude (local time) and latitude sectors (i.e. LT ~ 1030 1300, Dip Lat. ≤ 1.5°).
Achieving a good local time coverage is critical to ionospheric field modeling, if one wants to disentangle longitude, local time and seasonal dependence of the Sq and EEJ fields.
In this manner, Alken and Maus (2007) proposed an empirical model of EEJ climatological mean and day-to-day variability as a function of longitude, local time, season, and solar flux.
The climatological model provides the mean and variance of the EEJ as a function of longitude, local time, season, solar flux, and lunar local time (Alken and Maus 2007).
A systematic study of the EEJ characteristics using all the data from the Oersted, CHAMP, and SAC-C satellites obtained during the years (1999 to 2006) was used to construct the equatorial electrojet climatological model (EEJM-2.0) to reflect the day-to-day variability of electrojet using the input parameters of longitude, local time, and season and solar flux.
On the other hand, previous statistical analyses indicated that there are significant correlations between plasma bubble occurrences and F10.7 (Watanabe and Oya 1986; Huang et al. 2002; Nishioka et al. 2008), although the correlation depends on various parameters such as longitude, local time, and year.
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There has been attempt to predict longitude-local time distribution of scintillation based on the perceived role of gravity waves in initiating the bubble growth.
This observation, conducted on May 6, 2016, sampled the region of (longitude, latitude, local time, SZA) = (170°, 10°N, 17:14, 78°) during the ingress and the region of (longitude, latitude, local time, SZA) = (350°, 14°S, 05:102°102°) during the egress.
The geographical longitude and local noon of Himawari-8 and 9 are 140.7° and 02 37 UT, respectively.
The comparison shows that THM predictions agree in general with those of the other models, but THM variations along latitude, longitude and local time have larger amplitudes.
In this period, the geographic longitude and local noon of GOES 06 and 07 were 135.5° 21022 UT) and 108.5° 18144 UT), respectively.
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