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dc.contributor.author Nogueira, P. A. B.
dc.contributor.author Souza, J. R.
dc.contributor.author Abdu, M. A.
dc.contributor.author Paes, R. R.
dc.contributor.author Sousasantos, J.
dc.contributor.author Marques, M. S.
dc.contributor.author Bailey, G. J.
dc.contributor.author Denardini, C. M.
dc.contributor.author Batista, I. S.
dc.contributor.author Takahashi, H.
dc.contributor.author Cueva, R. Y. C.
dc.contributor.author Chen, S. S.
dc.date.accessioned 2018-11-15T15:50:21Z
dc.date.available 2018-11-15T15:50:21Z
dc.date.issued 2015-03-11
dc.identifier.citation Nogueira, P. A. B., Souza, J. R., Abdu, M. A., Paes, R. R., Sousasantos, J., Marques, M. S., ... Chen, S. S. (2015). Modeling the equatorial and low‐latitude ionospheric response to an intense X‐class solar flare.==$Journal of Geophysical Research: Space Physics, 120$==(4), 3021-3032. https://doi.org/10.1002/2014JA020823 es_ES
dc.identifier.uri http://hdl.handle.net/20.500.12816/3623
dc.description.abstract We have investigated the ionospheric response close to the subsolar point in South America due to the strong solar flare (X2.8) that occurred on 13 May 2013. The present work discusses the sudden disturbances in the D region in the form of high‐frequency radio wave blackout recorded in ionograms, the E region disturbances in the form of the Sq current and equatorial electrojet intensifications, and the enhancement and decay in the ionospheric total electron content (TEC) as observed by a network of Global Navigation Satellite Systems receivers, the last of these manifestations constituting the main focuses of this study. The dayside ionosphere showed an abrupt increase of the TEC, with the region of the TEC increase being displaced away from the subsolar point toward the equatorial ionization anomaly (EIA) crest region. The decay in the ΔTEC following the decrease of the flare EUV flux varied at a slower ratio near the EIA crest than at the subsolar point. We used the Sheffield University Plasmasphere‐Ionosphere Model to simulate the TEC enhancement and the related variations as arising from the flare‐enhanced solar EUV flux and soft X‐rays. The simulations are compared with the observational data to validate our results, and it is found that a good part of the observed TEC variation features can be accounted for by the model simulation. The combined results from model and observational data can contribute significantly to advance our knowledge about ionospheric photochemistry and dynamics needed to improve our predictive capability on the low‐latitude ionospheric response to solar flares. es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher American Geophysical Union es_ES
dc.relation.ispartof urn:issn:2169-9380
dc.rights info:eu-repo/semantics/restrictedAccess es_ES
dc.subject Ionospheric response to solar flare es_ES
dc.subject TEC disturbance es_ES
dc.subject Ionospheric modeling es_ES
dc.title Modeling the equatorial and low‐latitude ionospheric response to an intense X‐class solar flare es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#1.05.01 es_ES
dc.identifier.journal Journal of Geophysical Research: Space Physics es_ES
dc.description.peer-review Por pares es_ES
dc.identifier.doi https://doi.org/10.1002/2014JA020823 es_ES

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