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Day-to-day variability of equatorial anomaly in GPS-TEC during low solar activity period
Authors:Malini Aggarwal  HP Joshi  KN Iyer  Y-S Kwak  JJ Lee  H Chandra  KS Cho
Institution:1. Korea Astronomy and Space Science Institute, Daejeon 305-348, South Korea;2. Department of Physics, Saurashtra University, Rajkot 360-005, India;3. Physical Research Laboratory, Ahmedabad, India;4. NASA Goddard Space Flight Center, Greenbelt, MD, USA;5. Department of Physics, The Catholic University of America, Washington D.C., USA
Abstract:The ionospheric total electron content (TEC) in the northern hemispheric equatorial ionization anomaly (EIA) crest region is investigated by using dual-frequency signals of the Global Positioning System (GPS) acquired from Rajkot (Geog. Lat. 22.29°N, Geog. Long. 70.74°E; Geom. Lat. 14.21°N, Geom. Long. 144.90°E), India. The day-to-day variability of EIA characteristics is examined during low solar activity period (F10.7∼83 sfu). It is found that the daily maximum TEC at EIA crest exhibits a day-to-day and strong semi-annual variability. The seasonal anomaly and equinoctial asymmetry in TEC at EIA is found non-existent and weaker, respectively. We found a moderate and positive correlation of daily magnitude of crest, Ic with daily F10.7 and EUV fluxes with a correlation coefficient of 0.43 and 0.33, respectively indicating an existence of a short-term relation between TEC at EIA and the solar radiation even during low solar activity period. The correlation of daily Ic with Dst index is also moderate (r = −0.35), whereas no correlation is found with the daily Kp index (r = 0.14) respectively. We found that the magnitude of EIA crest is moderately correlated with solar flux in all seasons except winter where it is weakly related (0.27). The magnitude of EIA crest is also found highly related with EEJ strength in spring (r = 0.69) and summer (r = 0.65) than autumn (0.5) and winter (r = 0.47), though EEJ is stronger in autumn than spring.
Keywords:GPS-total electron content (TEC)  Equatorial ionization anomaly (EIA)  Equatorial electrojet (EEJ)
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