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The Impact of the Disturbed Electric Field in the Sporadic E (Es) Layer Development Over Brazilian Region
Author(s) -
Resende L. C. A.,
Shi J.,
Denardini C. M.,
Batista I. S.,
Picanço G. A. S.,
Moro J.,
Chagas R. A. J.,
Barros D.,
Chen S. S.,
Nogueira P. A. B.,
Andrioli V. F.,
Silva R. P.,
Carrasco A. J.,
de Araujo R. C.,
Wang C.,
Liu Z.
Publication year - 2021
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1029/2020ja028598
Subject(s) - ionosonde , electric field , ionosphere , dynamo , geomagnetic storm , wind shear , equatorial electrojet , geology , storm , atmospheric sciences , geophysics , physics , magnetic field , meteorology , earth's magnetic field , wind speed , plasma , electron density , quantum mechanics
During disturbed periods, E region electric fields can cause anomalous Es layer behavior, which is observed in the digital ionosonde data. To investigate the influence of these electric fields in the Es layer development, we analyzed a set of 20 magnetic storms from 2015 to 2018 over Boa Vista (BV, 2.8°N, 60.7°W, dip ∼18°), São Luís (SLZ, 2.3°S, 44.2°W, dip ∼8°), and Cachoeira Paulista (CXP, 22.41°S, 45°W, dip ∼35°). The electric field zonal components during the main and recovery phases of each magnetic storm are computed to study the corresponding characteristics of these Es seen in ionograms. Additionally, a numerical model (MIRE, Portuguese acronym for E Region Ionospheric Model) is used to analyze the Es layer dynamics modification around disturbed times. Using observation data and simulations, we were able to establish a threshold value for the electric field intensity for each region that can affect the Es layer formation. The results sustain that the strong Es layer in BV can be an indicator of the disturbed dynamo event. At SLZ, on the other hand, the Es layers are affected by the competition mechanisms of their formation, as equatorial electrojet irregularities and winds, during the main phase of the magnetic storm. Over CXP, the Es layer dynamics are dominated by the wind shear mechanism. Finally, this study provides new insights into the real impact of the electric field in the Es layer development over the Brazilian sector. Thus, our results lead to a better understanding of the underlying mechanisms related to the Es layer formation and dynamics.