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Characterization of seasonal and longitudinal variability of EEJ in the Indian region
Author(s) -
Phani Chandrasekhar N.,
Arora Kusumita,
Nagarajan Nandini
Publication year - 2014
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1002/2014ja020183
Subject(s) - daytime , equatorial electrojet , electrojet , climatology , atmospheric sciences , troposphere , earth's magnetic field , bay , geology , environmental science , physics , oceanography , quantum mechanics , magnetic field
Abstract This paper presents the seasonal and longitudinal variability of the equatorial electrojet (EEJ) based on geomagnetic variation data from two electrojet stations in the northern Indian Ocean at a longitudinal separation of ~15°: i.e., at 77°E and at 93°E. One complete year of data is used (i.e., from November 2011 to October 2012) at the two longitudes and compared with the climatological model of the equatorial electrojet (EEJM‐2.0). The results of our analysis show that (i) the monthly averaged hourly values of EEJ strength at 77°E and 93°E are overall in agreement with global characteristics of EEJ with significant departures over the year of study, (ii) the monthly average hourly daytime values at Campbell Bay and Vencode show poor correlation ( r < 0.7) for 5 out of 10 months, (iii) comparison of observed EEJ strength at respective longitudes and the current densities derived from EEJM‐2.0 show overall agreement with significant differences for monthly mean hourly daytime values at respective longitudes, and (iv) day‐to‐day variability in noontime EEJ amplitudes between the two longitudes is >10 nT, >20 nT for 30% of quiet days, sorted by planetary index ( Kp ) <1 and <2. This variability is reflected in monthly average values (V) mechanisms for persistent differences in EEJ on day‐to‐day basis are sought from perturbation of westward ion drifts by neutral winds caused by the upward propagation of gravity waves from troposphere/stratosphere into the mesosphere. These mechanisms have been identified theoretically and experimentally. The four‐wave structure of ionospheric current densities obtained by EEJM‐2.0 and other contemporary models closely resembles atmospheric tidal signatures and has a common origin. The magnitude and persistence of these differences, at short spatial scales (15°), are significant observation. These effects are reflected in the monthly and seasonal signatures of EEJ and contribute to the contemporary models.