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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/3RFJT55
Repositóriosid.inpe.br/mtc-m21c/2018/07.18.14.02
Última Atualização2021:01.04.18.30.06 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21c/2018/07.18.14.02.16
Última Atualização dos Metadados2021:01.04.18.30.07 (UTC) simone
Chave SecundáriaINPE--PRE/
Chave de CitaçãoMuralikrishna:2018:MeDuEf
TítuloMeteoric dust effects on the electrodynamics of low latitude e-region plasma
Ano2018
Data de Acesso12 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho60 KiB
2. Contextualização
AutorMuralikrishna, Polinaya
Identificador de Curriculo8JMKD3MGP5W/3C9JJ4G
GrupoDIDAE-CGCEA-INPE-MCTIC-GOV-BR
AfiliaçãoInstituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autorpolinaya.muralikrishna@inpe.br
Nome do EventoCospar Scientific Assembly, 42
Localização do EventoPasadena, California
Data14-22 July
Histórico (UTC)2018-07-18 14:02:30 :: simone -> administrator :: 2018
2019-01-18 02:41:37 :: administrator -> simone :: 2018
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoElectrodynamic processes occurring in the E-region of the equatorial ionosphere can be affected by dust particles of meteoric origin. The dust particles can capture the ambient electrons and cause considerable increase in the loss rate of electrons thus affecting the growth rates and amplitudes of the plasma irregularities. The attachment of electrons on dust particles can increase the threshold velocities needed for the onset of two stream and gradient drift instability mechanisms responsible for the generation of Type I and Type II plasma irregularities respectively, observed in the equatorial E-region plasma. In situ rocket observations also indicate that, under similar ambient conditions, the amplitudes of Type II irregularities observed in the lower E-region are considerably smaller than those observed at higher altitudes. This probably is a direct evidence for the effect of dust particles that dominate the lower E-region altitudes practically all the time. Electric field changes in the low latitude E-Region are attributed to changing neutral winds and to remote causes like the mapping of storm time electric field changes or changes in the neutral winds caused by Sudden Stratospheric Warming (SSW). Variation of electrojet currents is a manifestation of changing electric fields and/or electrical conductivities. Changes in the conductivity parameters, especially in the lower E-region can also be caused by the ambient dust particles of meteoric origin. Statistical studies have shown that the monthly occurrence rate of reversals in the electrojet currents is highly correlated to the monthly mean of meteor showers. This high correlation is seen even during geomagnetically disturbed periods. The meteoric dust particles thus play a very important role in altering the local electrical conductivities in the lower E-region and in controlling the electrodynamic processes in this region.
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Arquivo Alvomurali_meteoric.pdf
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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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