Morphology of GPS and DPS TEC over an equatorial station: validation of IRI and NeQuick 2 models
We investigated total electron content (TEC) at Ilorin (8.50∘ N 4.65∘ E, dip lat. 2.95) for the year 2010, a year of low solar activity in 2010 with Rz=15.8. The investigation involved the use of TEC derived from GPS, estimated TEC from digisonde portable sounder data (DPS), and the International Reference Ionosphere (IRI) and NeQuick 2 (NeQ) models. During the sunrise period, we found that the rate of increase in DPS TEC, IRI TEC, and NeQ TEC was higher compared with GPS TEC. One reason for this can be attributed to an overestimation of plasmaspheric electron content (PEC) contribution in modeled TEC and DPS TEC. A correction factor around the sunrise, where our finding showed a significant percentage deviation between the modeled TEC and GPS TEC, will correct the differences. Our finding revealed that during the daytime when PEC contribution is known to be absent or insignificant, GPS TEC and DPS TEC in April, September, and December predict TEC very well. The lowest discrepancies were observed in May, June, and July (June solstice) between the observed values and all the model values at all hours. There is an overestimation in DPS TEC that could be due to extrapolation error while integrating from the peak electron density of F2 (NmF2) to around ∼1000 km in the Ne profile. The underestimation observed in NeQ TEC must have come from the inadequate representation of contribution from PEC on the topside of the NeQ model profile, whereas the exaggeration of PEC contribution in IRI TEC amounts to overestimation in GPS TEC. The excess bite-out observed in DPS TEC and modeled TEC indicates over-prediction of the fountain effect in these models. Therefore, the daytime bite-out observed in these models requires a modifier that could moderate the perceived fountain effect morphology in the models accordingly. The daytime DPS TEC performs better than the daytime IRI TEC and NeQ TEC in all the months. However, the dusk period requires attention due to the highest percentage deviation recorded, especially for the models, in March, November, and December. Seasonally, we found that all the TECs maximize and minimize during the March equinox and June solstice, respectively. Therefore, GPS TEC and modeled TEC reveal the semiannual variations in TEC.
Total electron content (TEC) is the total number of free electrons in a columnar of 1 m2 along the radio path from the satellite to the receiver on the Earth. TEC exhibits diurnal, seasonal, solar cycle, and geographical variations. Therefore, the physical and dynamical morphology of the TEC over a given location is of great importance in transionospheric communications during both quiet and disturbed geomagnetic conditions (Aravindan and Iyer, 1990; Akala et al., 2012; Olawepo et al., 2015; Tariku, 2015 and de Jesus et al., 2016). GPS TEC is quantified from the GPS orbiting satellites to the GPS receiver station on the Earth, with an approximate distance of 20 200 km (Liu et al., 2006). Thus, a typical GPS TEC measurement incorporates the complete plasmaspheric electron content (PEC). The digisonde portable sounder (DPS) estimates the bottomside and topside TEC to obtain the total TEC from the electron density (Ne) profile. The topside DPS TEC is extrapolated from the peak electron density of the F2 region (NmF2) to around ∼1000 km; thus, the significant PEC contribution from the higher altitudes is omitted from DPS TEC measurement (Reinisch and Huang, 2001; Belehaki et al., 2004 and Zhang et al., 2006).
The International Reference Ionosphere (IRI) model depends on worldwide data from various measurements (Bilitza, 1986, 2000; Bilitza and Rawer, 1998). The IRI model provides reliable ionospheric densities, composition, temperatures, and composition in the ionospheric altitude range (Radicella et al., 1998; Bilitza, 2000 and Coisson et al., 2009). The latest version of the IRI model can be found at all time on the web (https://ccmc.gsfc.nasa.gov/modelweb/models/iri2016_vitmo.php; last access: 22 October 2018) with improvements on earlier versions of the model. The NeQuick 2 (NeQ) model makes use of the position, time and solar flux or sunspot number over a given location as variables in the NeQ model code (Coisson et al., 2006; Bidaine and Warnant, 2011 and Andreeva and Lokota, 2013). The output of the NeQ program and corresponding TEC are given by the electron density along any ray path and numerical integration in space and time respectively.
The availability of ionospheric parameters for global ionospheric models is deficient over the African sector compared to the consistent input of the data from the Asian and American sectors. Therefore, the continuing investigations of the parameters over Africa are required to improve the global ionospheric model. For example, Bagiya et al. (2009) studied TEC around an equatorial, low-latitude region at Rajkot (22.29∘ N, 70.74∘ E, dip 14.03∘ N) during low solar activity, Olwendo et al. (2012) and Karia and Pathak (2011) investigated the TEC data at Kenyan and Surat (India), respectively. They all noticed a semiannual variation with minimum and maximum TEC in the June solstice and March equinox, respectively. Using the Faraday rotational technique, Olatunji (1967) investigated TEC variation over the equatorial latitude at Ibadan. He observed no daytime bite-out and seasonal anomaly over the region. Rastogi et al. (1975) observed the diurnal variation of TEC using Faraday rotation over the magnetic equator. They noticed that TEC at the topside was higher than TEC at the bottomside during the nighttime; however, during the daytime they observed a uniform distribution of the TEC, on the topside and the bottomside of Ne profile.
Regarding the DPS TEC measurement, Barbas et al. (2010) examined GPS TEC and DPS TEC at Tucuman (26.69∘ S, 65.23∘ W) during different seasons. They inferred that the DPS TEC represented the GPS TEC with a minimal discrepancy in all seasons. Reinisch et al. (2004) investigated GPS TEC and DPS TEC in a mid-latitude and equatorial region. They observed that the variations in GPS TEC and DPS TEC appeared similar, but the daytime values of GPS TEC were higher than daytime DPS TEC. Zhang et al. (2004) studied the variations in DPS TEC and GPS TEC over Hainan and reported that the daytime DPS TEC and GPS TEC were similar in value during the daytime, but during the dusk period, they observed a significant discrepancy between DPS TEC and GPS TEC. Belehaki et al. (2004) extracted the PEC from the GPS TEC at Athens (38∘ N, 23.5∘ E) for over a year. They reported a maximum and minimum contribution of PEC in the morning and evening, respectively. Mosert et al. (2007), Jodogne et al. (2004) and McKinnell et al. (2007) concluded that approximated PEC from the GPS TEC and DPS TEC is possible in colocated GPS and DPS station. Adewale et al. (2012), Okoh et al. (2015), Jee et al. (2005), Kenpankho et al. (2013), Sulungu et al. (2018), and Migoya Orué et al. (2008) validated the IRI TEC with GPS TEC at different regions and found high discrepancies between the IRI TEC and GPS TEC when compared to different IRI-model options.
Cherniak and Zakharenkova (2016) validated the NeQ model. They established underestimation of the topside ionosphere above ∼500 km in the NeQ model, due to inaccurate representation of the topside Ne profile. Rabiu et al. (2014) validated the NeQ model using GPS TEC over the equatorial region of Africa. They reported that the upper boundary of the NeQ model, up to 20,000 km, needed to be adjusted to accommodate the PEC TEC in the NeQ model. Leong et al. (2015) investigated TEC and the NeQ model. They found that the observed and NeQ TEC were similar in value during dusk periods, but the changed TEC revealed higher discrepancies postsunset. Yu et al. (2012) investigated the monthly average of NeQ TEC model over three stations in China (Changchun, Beijing, and Chongqing) during the quietest period (i.e. days with Ap ≤4). They revealed that NeQ correctly predicted GPS TEC. However, the NeQ TEC underestimated the GPS TEC during the dusk period. Rios et al. (2007) investigated the variations in DPS TEC and IRI TEC and found that DPS TEC was smaller compared to IRI TEC. McNamara (1985) observed discrepancies between DPS TEC and IRI TEC and found that the IRI underestimated the DPS TEC during the daytime. Obrou et al. (2008) compared the DPS TEC and IRI TEC at Korhogo during high and low solar activity. They found that the variations in DPS TEC and IRI TEC were similar in value during high solar activity (HSA) and low solar activity (LSA), but the performance of IRI TEC was better during HSA compared to LSA.
The current contributions of Africa to the improvement of ionospheric models (IRI and NeQuick) are not adequate compared with the continuous support received from Asia and South America. The insufficient instrumentation at the equatorial region of Africa has a considerable effect on this shortcoming. Therefore, the constant validation of IRI and models with the observed parameter is necessary for an improved ionospheric model. Furthermore, the investigation on DPS TEC has not been reported extensively for comparison purposes over the equatorial region of Africa. Therefore, this study investigates the linked morphologies between the variations in GPS TEC and DPS TEC as well as validations of IRI TEC and NeQ TEC models with the observed parameters. Our finding will inform the suitability of modeled TEC in place of GPS TEC. The result will also determine the appropriate model for the equatorial latitude in Africa. Thus, the deviations in TEC obtained from the combined relationship between GPS TEC, DPS TEC, IRI TEC, and NeQ TEC could be used to correct the discrepancy in the models.
Data used for this study are those of the five quietest days of each month of the year 2010. The five quietest days are days (with Ap ≤4) for which geomagnetic activities are quiet, which are obtained from the international quiet day (IQD) table available on the website of Geoscience Australia. The data are for Ilorin (8.50∘ N 4.65∘ E, dip lat. 2.95) during the year 2010, a year of low solar activity. TEC data were obtained with a GPS receiver and DPS, both of which are located at the Ionospheric Laboratory of the University of Ilorin. The methods of data processing are described in the sections below.
2.1 GPS TEC
The slant TEC records from GPS have errors due to satellite differential delay (satellite bias (bS)), receiver differential delay (receiver bias (bR)), and receiver interchannel bias (bSR). This uncorrected slant GPS TEC, measured at every 1 min interval by the GPS receiver and derived from all the visible satellites at Ilorin station, are converted to vertical GPS TEC using the relation below in Eq. (1).
where (GPSTEC)S is the uncorrected slant GPS TEC measured by the receiver, S(E) is the obliquity factor with zenith angle (z) at the ionospheric pierce point (IPP), E is the elevation angle of the satellites in degrees, and (GPSTEC)V is the vertical GPS TEC at the IPP. The equation two below provides S(E) as
where RE is the mean radius of the Earth measured in kilometer (km), and hS is the height of the ionosphere from the surface of the Earth, which is approximately equal to 400 km according to Langley et al. (2002), Rama Rao et al. (2006a), and Mannucci et al. (1993). The data from the five quietest slant GPS TEC days for each month in the year 2010 were interpreted using Krishna software (Global positioning system total electron content analysis application user's manual, 2009, Institute for Scientific Research, Boston College, Chestnut Hill, Massachusetts, USA). This software reads raw data and corrects all source of errors mentioned above from Global Navigation Satellite System (IGS) service code file. A minimum elevation angle of 20∘ is used to avoid multipath errors. The estimated vertical GPS TEC data are a function of a two-sigma (2σ) iteration. This sigma is a measure of GPS point positioning accuracy. We converted the average 1 min VTEC data to hourly averages.
2.2 DPS TEC
Regarding the TEC from the DPS, the Standard Archive Output (SAO) files obtained from the DPS at the University of Ilorin were edited to remove magnetically disturbed days. Huang and Reinisch (2001) technique was used to compute the DPS TEC. The vertical DPS TEC computation by the technique is based on the application of the integration over the vertical electron density [Ne(h)] profile as shown in the Eq. (3) below.
where and are the bottomside and topside Ne profiles, respectively. We computed the NeB from the recorded ionograms by using the inversion technique developed by Huang and Reinisch (1996a, b). The information above the peak of the F2 layer is absent from the record of the ionogram. Thus, the is measured by approximating the exponential functions with suitable scale height (Bent et al., 1972) with a lower estimated error of 5 %. The ionograms were manually scaled and inverted into electron density profiles using the NHPC software and later processed with the SAO explorer software based on the technique described above to obtain the TEC (Reinisch et al., 2005). We estimated an average of TEC for each hour over the selected days. Universal time (UT) is the time standard for the record of GPS and DPS data, but we converted UT to local time (LT) by adding 1 h to the corresponding UT. Nigeria is 1 h in advance of Greenwich mean time (GMT); thus, 01:00 UT is the same as 02:00 LT in Ilorin, Nigeria. The available months of the year were grouped into seasons in order to study the seasonal variation of TEC and the performances of some of the options in the IRI model. The four seasons are grouped as March equinox or MEQU (March and April), June solstice or JSOL (June and July), September equinox or SEQU (September and October) and December solstice or DSOL (November and December). The monthly median of the five quietest days were deduced and the average of the monthly median under a particular season as defined above to infer seasonal variations under GPS TEC, DPS TEC, IRI TEC, and NeQ TEC. The DPS in Ilorin was installed in March, 2010, as a result data were not available for the months of January to late March, 2010. Therefore, this study does not include the days for which DPS data were not available.
2.3 Validation of IRI – 2016 and NeQuick 2 models
We correlated the observed TEC with modeled TEC in the IRI-2016 model. The website https://ccmc.gsfc.nasa.gov/modelweb/models/iri2016_vitmo.php (last access: 22 October 2018) provides the modeled TEC values. We selected the upper boundary height 2000 km and the B0 table option for the bottomside shape parameter. The Eqs. (4a–c) represent the differences between GPS TEC and DPS TEC, GPS TEC and IRI TEC, and GPS TEC and NeQ TEC while Eqs. (5a–c) below show the percentage change between GPS TEC and DPS TEC, GPS TEC and IRI TEC, and GPS TEC and NeQ TEC.
ΔDPS−GPS, ΔIRI−GPS, and ΔNeQ−GPS represent the difference between GPS TEC and DPS TEC, GPS TEC and IRI TEC, and GPS TEC and NeQ TEC, respectively, while %(ΔDPS−GPS), %(ΔIRI−GPS), and %(ΔNeQ−GPS) represent the percentage deviation between GPS TEC and DPS TEC, GPS TEC and IRI TEC, and GPS TEC and NeQ TEC, respectively.
The Abdus Salam International Centre for Theoretical Physics (ICTP) in Trieste, Italy, in collaboration with the Institute for Geophysics, Astrophysics and Meteorology (IGAM) of the University of Graz, Austria, developed the web front end of NeQuick. This quick-run ionospheric electron density model developed at the Aeronomy and Radiopropagation Laboratory modeled TEC along any ground-to-satellite straight-line ray path. Therefore, we validated the NeQ obtained from https://t-ict4d.ictp.it/nequick2/nequick-2-web-model (last access: 22 October 2018).
3.1 Monthly median variations in GPS and modeled TEC
Figure 1a shows the simultaneous plots of hourly variations in the monthly median of TEC obtained from GPS,DPS, IRI, and NeQ TEC during the quiet period. The GPS TEC is denoted by a black line with the star symbol; the DPS TEC is denoted by a green line with the diamond symbol, IRI TEC is denoted by a red line with zero symbols, and finally, the NeQ TEC is denoted by a blue line with multiplication symbols. All the TEC plots are regulated by the same local time on the horizontal axis. The result reveals that the morphologies of GPS, DPS, and modeled TEC increase gradually from the sunrise period (07:00–09:00 LT) and reach the daytime maximum, mostly around (12:00–17:00 LT), and then later decay steadily until a minimum value around 06:00 LT. Therefore, our result suggests that the diurnal variations in the observed and modeled TEC capture the well known solar zenith angle dependence of TEC since both observed and modeled TEC characterize presunrise minimum, daytime maximum, daytime depression (modeled TEC), and postsunset decay. The lowest and highest presunrise minimum ranged from ∼0.66 to ∼4.49 TECU (DPS) while the lowest and highest daytime maximum found between ∼17.75 TECU (NeQ) and ∼38.0 TECU (DPS). The result shows noontime bite-out in modeled TEC around 12:00 and 15:00 LT, except in GPS TEC where the bite-out was obscure apart from a slight shift in daytime maximum within 15:00 and 17:00 LT in all months. We observed two moderate peaks (prenoon and postnoon peaks) in DPS TEC and modeled TEC, indicating the bite-out effect on the modeled and DPS TEC signatures. We also found around the sunrise period, the model TEC rises faster than the GPS TEC, but IRI TEC rises faster compared to DPS TEC and NeQ TEC. Between 06:00 and 09:00 LT, the lowest and highest differences in the rises of IRI TEC compared to GPS TEC were ∼5.0 TECU (March) and ∼15.3 TECU (November), respectively. The postnoontime decay was faster in DPS TEC compared to GPS TEC and modeled TEC in all months. Figure 1b reveals the coincident seasonal variations in GPS, DPS, and modeled TEC during a quiet period of the (i) March equinox, (ii) June solstice, (iii) September equinox, and (iv) December solstice. The daytime maximum ranges are from ∼24.8 TECU (NeQ) to ∼34 TECU (DPS), ∼19.2 TECU (NeQ) to ∼22.6 TECU (DPS), ∼24.9 TECU (NeQ) to ∼33.5 TECU (DPS), and ∼24.55 TECU (NeQ) to ∼31 TECU (DPS), during the March equinox, June solstice, September equinox, and December solstice, respectively. We observed that the morphologies of GPS TEC and modeled TEC maximize and minimize during the March equinox and June solstice, thus indicating semiannual variation in observed and modeled TEC.
3.2 Percentage deviation of DPS TEC, IRI TEC, and NeQ TEC
Figures 2a, 3a, and 4a are hourly variations in deviation in TEC (ΔTEC) between GPS-, DPS-, IRI- and NeQ-derived TEC whereas Figs. 2b, 3b, and 4b depict the mass plots of hourly variations in the percentage deviation (%ΔTEC) during a quiet period from March to December. In Fig. 2a and b, the overestimation by DPS TEC as given by ΔTECDPS−GPS is within the range of ∼5.13 TECU (March) to ∼19.12 TECU (July) around 07:00–16:00 LT while the underestimation ΔTECDPS−GPS fluctuated between ∼3.2 TECU (June) and ∼16.4 TECU (November) around 17:00–24:00 LT. The overestimation and underestimation of %ΔIRI−GPS ranged from ∼2 % to ∼49 % and % to %, respectively. From Figs. 3a and b, the overestimation occurred regularly around 04:00–12:00 LT in all months. The overestimated and underestimated ΔTECIRI−GPS were from ∼9.13 TECU (July) to ∼15.3 TECU (November) and ∼0.15 TECU (October) to ∼0.95 TECU (July), respectively. However, a few underestimations and overestimations of ΔTECIRI−GPS still occurred irregularly around 13:00–03:00 LT in all months. The result also shows that IRI TEC completely overestimated GPS TEC in May and June between 01:00 and 24:00 LT. The overestimation of %ΔTECIRI−GPS ranged between ∼0.1 % and ∼86 % in all months. In Figs. 4a and b, NeQ TEC overestimated GPS TEC at 01:00–11:00 and 20:00–24:00 LT with ΔTECNeQ−GPS ranging from ∼9.72 (September) to ∼0.01 (April). We also found that NeQ TEC underestimated ΔTECNeQ−GPS by between ∼0.11 (May) and ∼9.72 (November). The overestimations and underestimations of %ΔTECNeQ−GPS are from ∼0.02 % to ∼81 % and % to % respectively.
3.3 Comparisons of the percentage deviations from GPS TEC
In Figs. 2b, 3b, and 4b, the percentage deviation between GPS and DPS TEC are more significant: greater than 100 % in March–August, September, November, and December at 04:00–05:00 LT and around 22:00–24:00 LT in June and July. The percentage deviation between GPS and IRI TEC is also lower than 100 %, except in March at around 04:00 LT, whereas the difference between GPS and IRI TEC is greater than 100 %. The percentage deviations in DPS and modeled TEC during dusk periods are always higher than their corresponding deviations during the daytime. During the daytime, the deviations are smaller in DPS and NeQ TEC compared to IRI TEC.
An investigation into the variations in GPS TEC, DPS TEC, and the validations of modeled TECs in an equatorial region (8.50∘ N, 4.650∘ E) in Africa during low solar activity in the year 2010 has been carried out. The TEC increases gradually from the sunrise period, then slowly reaches the daytime maximum, and later decays to the presunrise minimum. This result indicates that the observed and modeled TEC are a solar zenith angle dependence showing peak and lowest TEC values during noontime and dusk, respectively (Aravindan and Iyer, 1990; Wu et al., 2008 and Kumar and Singh, 2009). Interestingly, our result reveals that the faster rise in the DPS TEC compared to GPS TEC during sunrise is not consistent with the findings of Ezquer et al. (1992) at Tucumán (26.9∘ S; 65.4∘ W), Belehaki et al. (2004) at Athens, McNamara (1985) at low latitude, and Obrou et al. (2008) at Korhogo (9.33∘ N, 5.43∘ W, Dip =0.67∘ S). They all found that the GPS TEC increased faster than the DPS TEC during the sunrise. The enrichment of PEC on TEC latterly reported by Belehaki et al. (2004) indicated a significant PEC increase in the morning and dusk time. Recently, Jodogne et al. (2004), Mosert et al. (2007), and McKinnell et al. (2007) also obtained a rough estimation of PEC from the GPS and DPS TEC variations. They inferred that the combined GPS TEC and DPS TEC could give the PEC contribution in TEC of a given location. Therefore, the higher rise in DPS TEC compared to GPS TEC during the sunrise in our study could be attributed to inaccurate representation of PEC in the topside DPS TEC profile and incurred error during the extrapolation of the Ne profile from the peak of F2 region (NmF2) to ∼1000 km. Therefore, a typical TEC measurement naturally includes a meaningful PEC contribution (Balan and Iyer, 1983; Carlson, 1996; Breed et al., 1997; and Belehaki et al., 2005).
The higher values in DPS TEC compared with IRI TEC around sunrise is not consistent with Rios et al. (2007), who investigated the comparison of DPS TEC and IRI TEC. They found that DPS TEC is smaller than IRI TEC at all hours. They assumed that the prediction of IRI TEC had included the high topside Ne profile. Thus, our observation may suggest that the IRI TEC has incorporated low topside Ne profile in the IRI model or the excessive enhancement of PEC contribution in the topside Ne profile in the DPS TEC.
The similarity observed during daytime between GPS TEC and DPS TEC in April, August, and December may also suggest that the topside Ne profile in GPS TEC is accurate in the DPS TEC topside profile due to the absence of or negligible PEC contribution in DPS TEC values. The insignificant daytime PEC observed in this study is consistent with Rastogi et al. (1971) and Belehaki et al. (2004). Higher daytime DPS TEC compared with daytime IRI TEC is consistent with the result of McNamara (1985). However, Obrou et al. (2008) found, at the equatorial latitude, higher IRI TEC relative to DPS TEC during low solar activity. Therefore, the reduced daytime IRI TEC compared to GPS TEC values indicates the excessive PEC removal from the model values that its PEC contribution had been raised initially during the sunrise.
Also, the reduced NeQ TEC compared to GPS TEC values in all months is consistent with the reports of Migoya-Orue et al. (2017), Cherniak and Zakharenkova (2016), Rabiu et al. (2014), and Coisson et al. (2009). They recommended an added PEC contribution on the topside NeQ profile for an accurate prediction of the NeQ model.
The daytime bite-out in TEC is due to the occurrence of the most active fountain effect during noontime at the magnetic equator. The bite-out results from the vertical plasma drift due to the combined consequence of mutually perpendicular electric and magnetic fields on the plasma. The drift lifts the plasma at the magnetic equator and diffuses along geomagnetic field lines into the high latitudes, thereby leaving the reduced TEC at the magnetic equator (Bandyopadhyay, 1970; Skinner, 1966; Bolaji et al., 2012; Olwendo et al., 2013). However, the absence of daytime bite-out (Olatunji, 1967) in GPS TEC in our finding may be due to the greater amount of production at the bottomside and topside electron content that are enhanced quickly to replenish the loss of the ionization that occurs through the fountain effect during noontime.
The percentage difference between observed and modeled TEC reveals that the presunrise values in DPS TEC, IRI TEC, and NeQ TEC require modifications, especially during the month of March for DPS TEC and the models and November and December for DPS TEC only. The daytime DPS TEC is closer to the GPS TEC value compared to the daytime IRI TEC and NeQ TEC values. The nighttime NeQ TEC and IRI TEC perform better with GPS TEC compared with DPS TEC in all months. There is also the need to minimize the discrepancies observed during the dusk periods.
Seasonally, we found that TEC maximizes and minimizes during the equinoxes and the solstices, respectively. Our report is consistent with Bagiya et al. (2009), Wu et al. (2008), Kumar and Singh (2009), and Balan and Rao (1984), who investigated TEC in various regions. They attributed the seasonal variation in TEC to the seasonal differences in thermospheric composition. Moreover, the subsolar point is around the equator during the equinox. Consequently, the sun shines directly over the equatorial latitude, and in addition to the high ratio of O ∕ N2 around the region, this translates to stronger ionization and generates a semiannual variation in TEC. The finding from our study is consistent with the reports of Skinner (1966), Bolaji et al. (2012), and Scherliess and Fejer (1999), who obtained semiannual variation in TEC. Scherliess and Fejer (1999) also concluded that daytime E×B drift velocity could result in semiannual variation because the drift is more and less significant in the equinoctial months and June solstice, respectively.
We have examined the variations in observed and modeled TEC over an equatorial region in Africa during a year of low solar activity. Our findings showed the following:
GPS TEC and modeled TEC dependence on solar zenith angle;
a faster sunrise increase in the modeled TEC relative to GPS TEC, which suggests an overestimation of the topside Ne profile of the modeled TEC due to plasmaspheric electron content (PEC) in the models;
a good representation of the daytime measured TEC by the models, suggesting that the model TEC could represent GPS TEC in the absence of plasmaspheric TEC contribution;
that the ΔTECIRI−GPS and %ΔTECIRI−GPS in May and June consistently show overestimations at 01:00–24:00 LT, indicating the enhanced contribution of PEC at all hours in May and June;
that the percentage deviations in DPS and modeled TEC relative to GPS TEC during dusk periods is always higher than their corresponding differences during the daytime, and the values of daytime deviation in DPS and NeQ TEC are smaller compared to daytime deviation in IRI TEC.
This study was carried out during low solar activity in the year 2010; it will be of advantage to investigate and compare similar reviews during high solar activity with our results.
The GPS and DPS data are provided by the University of Ilorin, Nigeria, through the archived records of GPS and DPS observatories. The IRI and NeQuick model dataset is available on the websites https://ccmc.gsfc.nasa.gov/modelweb/models/iri2016_vitmo.php (Community Coordinated Modeling Cente, 2016) and https://tict4d.ictp.it/nequick2/nequick-2-web-mode (Abdus Salam International Centre for theoretical Physics, 2018), respectively.
OOO carried out the analysis and prepared the paper. JA, OO, OO, IA and EO participated in discussing the results, read the paper, and commented on it.
The authors declare that they have no conflict of interest.
The authors thank the US Air Force and Lowell Digisonde, Massachusetts, for
the donation and continual maintenance of the DPS. We also appreciate Boston
College and the SCINDA group for the donations and continual maintenance of
the GPS receiver at the University of Ilorin, Nigeria. We also appreciate
the support of the University of Ilorin and CAR-NASRDA for their support in
funding of the ionospheric observatories.
Edited by: Ana G. Elias
Reviewed by: Kavutarapu Venkatesh and one anonymous referee
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