Estimation of nighttime dip-equatorial E-region current density using measurements and models. (August 2016)

• Record Type: Journal Article
• Authors: Pandey, Kuldeep; Sekar, R.; Anandarao, B.G.; Gupta, S.P.; Chakrabarty, D.
• Is Part Of: Journal of atmospheric and solar-terrestrial physics. Volume 146(2016)
• Page Start: 160
• Page End: 170
• Publication Date: 2016-08
• Subjects: Equatorial ionosphere -- Equatorial electrojet -- Streaming plasma waves; Geophysics -- Periodicals; Atmospheric physics -- Periodicals; Géophysique -- Périodiques; Météorologie physique -- Périodiques; Electronic journals; 551.51
• DOI: 10.1016/j.jastp.2016.06.002
• Languages: English
• ISSNs: 1364-6826

Abstract

Abstract: The existence of the possible ionospheric current during nighttime over low-equatorial latitudes is one of the unresolved issues in ionospheric physics and geomagnetism. A detailed investigation is carried out to estimate the same over Indian longitudes using in situ measurements from Thumba ( 8.5 ° N, 76.9 ° E ), empirical plasma drift model (Fejer et al., 2008 ) and equatorial electrojet model developed byAnandarao (1976) . This investigation reveals that the nighttime E-region current densities vary from ∼0.3 to ∼0.7 A/km 2 during pre-midnight to early morning hours on geomagnetically quiet conditions. The nighttime current densities over the dip equator are estimated using three different methods (discussed in methodology section) and are found to be consistent with one another within the uncertainty limits. Altitude structures in the E-region current densities are also noticed which are shown to be associated with altitudinal structures in the electron densities. The horizontal component of the magnetic field induced by these nighttime ionospheric currents is estimated to vary between ∼2 and ∼6 nT during geomagnetically quiet periods. This investigation confirms the existence of nighttime ionospheric current and opens up a possibility of estimating base line value for geomagnetic field fluctuations as observed by ground-based magnetometer.