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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZGivnK2Y/RNVTS
Repositóriosid.inpe.br/mtc-m17@80/2007/10.19.20.42   (acesso restrito)
Última Atualização2007:11.27.11.54.47 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m17@80/2007/10.19.20.43.02
Última Atualização dos Metadados2021:07.18.04.01.34 (UTC) administrator
Chave SecundáriaINPE-14987-PRE/9898
ISSN1364-6826
Chave de CitaçãoLucasGEGLSVS:2007:EnBaDu
TítuloEnergy Balance during Intense and Super-Intense Magnetic Storms using an Akasofu Epsilon Parameter Corrected by The Solar Wind Dynamic Pressure
Ano2007
Data de Acesso28 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho757 KiB
2. Contextualização
Autor1 Lucas, Aline de
2 Gonzalez, Walter Demé
3 trio
4 Echer, Ezequiel
5 Guarnieri, Luis Fernando
6 Lago, Alisson Dal
7 Silva, Marlos Rockenbach da
8 Vieria, Luis Eduardo Antunes
9 Schuch, Nelson Jorge
Identificador de Curriculo1
2
3
4 8JMKD3MGP5W/3C9JH3D
5
6 8JMKD3MGP5W/3C9JGH3
7
8
9 8JMKD3MGP5W/3C9JHUD
Grupo1 DGE-INPE-MCT-BR
2 DGE-INPE-MCT-BR
3 DGE-INPE-MCT-BR
4 DGE-INPE-MCT-BR
5 DGE-INPE-MCT-BR
6 DGE-INPE-MCT-BR
7 DGE-INPE-MCT-BR
8 RSU-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Instituto Nacional de Pesquisas Espaciais (INPE)
8 Centro Regional Sul de Pesquisas Espaciais (CRS/INPE)
RevistaJournal of Atmospheric and Solar-Terrestrial Physics
Volume69
Número15
Páginas1851-1863
Histórico (UTC)2007-12-19 14:19:02 :: martaseeger -> administrator ::
2021-07-18 04:01:34 :: administrator -> martaseeger :: 2007
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveSuper-intense magnetic storms
Energy transfer
å parameter
ResumoGeomagnetic storms are large disturbances in the Earth's magnetosphere caused by enhanced solar windmagnetosphere energy transfer. One of the main manifestations of a geomagnetic storm is the ring current enhancement. It is responsible for the decrease in the geomagnetic field observed at ground stations. In this work, we study the ring current dynamics during two different levels of magnetic storms. Thirty-three events are selected during the period 19812004. Eighteen out of 33 events are very intense (or super-intense) magnetic storms (Dst −250 nT) and the remaining are intense magnetic storms (−250<Dst −100 nT). Interplanetary data from spacecraft in the solar wind near Earth's orbit (ACE, IMP-8, ISEE-3) and geomagnetic indices (Dst and Sym-H) are analyzed. Our aim is to evaluate the interplanetary characteristics (interplanetary dawndusk electric field, interplanetary magnetic field component BS), the å parameter, and the total energy input into the magnetosphere (Wå) for these two classes of magnetic storms. Two corrections on the å energy coupling function are made: the first one is an already known correction in the magnetopause radius to take into account the variation in the solar wind pressure. The second correction on the Akasofu parameter, first proposed in this work, accounts for the reconnection efficiency as a function of the solar wind ram pressure. Geomagnetic data/indices are also employed to study the ring current dynamics and to search for the differences in the storm evolution during these events. Our corrected å parameter is shown to be more adequate to explain storm energy balance because the energy input and the energy dissipated in the ring current are in better agreement with modern estimates as compared with previous works. For super-intense storms, the correction of the Akasofu å is on average a scaling factor of 3.7, whilst for intense events, this scaling factor is on average 3.4. The injected energy during the main phase using corrected å can be considered a criterion to separate intense from very intense storms. Other possibilities of cutoff values based on the energy input are also investigated. A threshold value for the input energy is much more clear when a new classification on Dst=−165 nT is considered. It was found that the energy input during storms with Dst<−165 nT is double of the energy for storms with Dst>−165 nT.
ÁreaCEA
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Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo AlvoEnergy balance during.pdf
Grupo de Usuáriosadministrator
martaseeger
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EU29DP
8JMKD3MGPCW/3EUFCFP
DivulgaçãoWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Acervo Hospedeirolcp.inpe.br/ignes/2004/02.12.18.39
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi e-mailaddress electronicmailaddress format isbn label lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
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