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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/3QTFMU2
Repositóriosid.inpe.br/mtc-m21c/2018/04.16.14.15
Repositório de Metadadossid.inpe.br/mtc-m21c/2018/04.16.14.15.20
Última Atualização dos Metadados2020:12.07.21.11.29 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoCandidoBatiRese:2018:IoReRe
TítuloIonospheric response to a recurrent magnetic storm during an event of High Speed Stream in October 2016
Ano2018
Data de Acesso13 maio 2024
Tipo SecundárioPRE CI
2. Contextualização
Autor1 Candido, Cláudia Maria Nicoli
2 Batista, Inez Staciarini
3 Resende, Laysa Cristina Araújo
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHDA
Grupo1 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
2 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
3 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 claudia.candido@inpe.br
2 inez.batista@inpe.br
Nome do EventoLatin American Conference on Space Geophysics, 11 (COLAGE)
Localização do EventoBuenos Aires, Argentina
Data16-20 abr.
Histórico (UTC)2018-04-16 14:15:32 :: simone -> administrator :: 2018
2018-04-18 05:03:02 :: administrator -> administrator] :: 2018
2018-04-18 05:03:02 :: administrator] -> administrator :: 2018
2019-01-04 16:57:04 :: administrator -> simone :: 2018
2019-01-07 12:59:09 :: simone -> administrator :: 2018
2020-12-07 21:11:29 :: administrator -> simone :: 2018
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoIn this work we investigate the response of the low latitude ionosphere to recurrent geomagnetic activity caused by events of High speed streams (HSSs)/Corotating Interaction Regions (CIRs) during the low descending phase of solar activity in the solar cycle 24. Intense magnetic field regions called Corotating Interaction Regions or CIRs are created by the interaction of fast streams and slow streams ejected by long duration coronal holes in Sun. This interaction leads to an increase in the mean interplanetary magnetic field (IMF) which causes moderate and recurrent geomagnetic activity when interacts with the Earths magnetosphere. The ionosphere can be affected by these phenomena by several ways, such as an increase (or decrease) of the plasma ionization, intensification of plasma instabilities during post-sunset/post-midnight hours and subsequent development of plasma irregularities/spreadF, as well as occurrence of plasma scintillation. Therefore, we investigate the low latitude ionospheric response during moderate geomagnetic storm associated to an event of High Speed Stream occurred during decreasing phase of solar activity in 2016. An additional ionization increasing is observed in Es layer during the main peak of the geomagnetic storm. We investigate two possible different mechanisms that caused these extras ionization: the role of prompt penetration of interplanetary electric field, IEFEy at equatorial region, and the energetic electrons precipitation on the E and F layers variations. Finally, we used data from Digisondes installed at equatorial region, Sao Lu´ıs, and at conjugate points in Brazilian latitudes, Boa Vista and Cachoeira Paulista. We analyzed the ionospheric parameters such as the critical frequency of F layer, foF2, the F layer peak height, hmF2, the F layer bottomside, hF, the blanketing frequency of sporadic layer, fbEs, the virtual height of Es layer hEs and the top frequency of the Es layer ftEs during this event.
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ETL868
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
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