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Characteristics of low‐latitude TEC during solar cycles 23 and 24 using global ionospheric maps (GIMs) over Indian sector
Author(s) -
Dashora N.,
Suresh Sunanda
Publication year - 2015
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1002/2014ja020559
Subject(s) - total electron content , tec , ionosphere , equator , solar minimum , low latitude , anomaly (physics) , solar cycle , atmospheric sciences , latitude , context (archaeology) , environmental science , climatology , physics , geology , geophysics , astronomy , condensed matter physics , quantum mechanics , magnetic field , solar wind , paleontology
Abstract The characteristics of quiet time equatorial and low‐latitude total electron content over the Indian sector using global ionospheric map (GIM) data (1998–2014) are obtained filtering out the solar flare and storm effects. The results are examined and interpreted in the context of large number of previous studies. The newly found features from this study are as follows. Marked difference in nature of equinoctial asymmetry is noted between solar cycles 23 and 24. Long absence of winter anomaly both during low and high solar activity (HSA) in LL (low‐latitude) regions is found. Climatology of the diurnal cycle is provided in four categories using new criteria for demarcation of solar activity levels. Highest correlation (~77%) between GIM ionospheric electron content (IEC) and PI (solar EUV proxy index) is noted over equator in contrast to previous studies. The minimum positive contribution of PI in variation of IEC requires minimum of 2 years of data, and if more than 7–8 years of data are used, it saturates. Root‐mean‐square width of PI can be used to define the HSA. Strong QBO (quasi‐biennial oscillations) in IEC is noted in tune with the one in PI over both LL locations but QBO remains surprisingly subdued over equator. The semiannual oscillations in GIM‐IEC are found to be stronger at all locations during high solar activity and weaker between 2005 and 2011, whereas the annual oscillations are found to be substantially stronger only during HSA‐23 and weakest over southern LL location throughout 17 years.

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