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(Referência obtida automaticamente do Web of Science, por meio da informação sobre o financiamento pela FAPESP e o número do processo correspondente, incluída na publicação pelos autores.)

On the ionospheric and thermospheric response of solar flare events of 19 January 2005: An investigation using radio and optical techniques

Texto completo
Autor(es):
Sumod, S. G. [1, 2] ; Pant, Tarun Kumar [1] ; Vineeth, C. [1] ; Hossain, M. M. [1]
Número total de Autores: 4
Afiliação do(s) autor(es):
[1] Indian Space Res Org, Space Phys Lab, Trivandrum, Kerala - India
[2] Univ Vale do Paraiba UNIVAP, Sao Paulo - Brazil
Número total de Afiliações: 2
Tipo de documento: Artigo Científico
Fonte: JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS; v. 119, n. 6, p. 5049-5059, JUN 2014.
Citações Web of Science: 2
Resumo

This study presents optical signatures of thermospheric OI 630.0nm dayglow variability over a geomagnetic dip equatorial station Trivandrum (8.5 degrees N, 77 degrees E, 0.5 degrees dip latitude), India, in response to solar flares of different ranks that occurred on 19 January 2005. It is found that over equator, the response of thermospheric dayglow to solar flares can be either prompt or delayed depending upon rank of the flare and dominant neutral/electrodynamical processes prevailing in the emission altitudes. This is strikingly in contrast to the earlier results, where prompt response of equatorial OI 630.0nm dayglow to solar flares has been noticed. In addition, the flare-induced changes at the E and F regions of the equatorial ionosphere are studied using high-cadence measurements of the equatorial electrojet (EEJ) and total electron content (TEC) obtained from the ground-based magnetometers and GPS receivers, respectively. The Hall/Pedersen conductivity measurements as inferred using the magnetometers over the EEJ station and an off-EEJ station showed concomitant changes during these flares. Although, the GPS-measured TEC showed prompt enhancement associated with these flares, the evolution of the equatorial ionization anomaly, as seen in the TEC did not show any flare-induced changes. The plausible mechanisms explaining these observations are adduced in context of the present understanding of the equatorial electrodynamics and its imprint on these dayglow features. (AU)

Processo FAPESP: 13/25037-4 - Estudo da camada F3 e dos efeitos do aquecimento estratosférico repentino na ionosfera em baixas latitude e região equatorial, durante o ciclo solar 24
Beneficiário:Sukumaran Nair Geetha Kumari Sumod
Modalidade de apoio: Bolsas no Brasil - Pós-Doutorado