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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34T/49C8QJH
Repositóriosid.inpe.br/mtc-m21d/2023/06.28.15.52
Última Atualização2023:06.28.15.52.42 (UTC) self-uploading-INPE-MCTI-GOV-BR
Repositório de Metadadossid.inpe.br/mtc-m21d/2023/06.28.15.52.42
Última Atualização dos Metadados2024:01.02.17.16.44 (UTC) administrator
DOI10.5194/acp-23-6145-2023
ISSN1680-7316
1680-7324
Rótuloself-archiving-INPE-MCTIC-GOV-BR
Chave de CitaçãoLiuXuYueAndr:2023:VaGlZo
TítuloVariations in global zonal wind from 18 to 100 km due to solar activity and the quasi-biennial oscillation and El Nino-Southern Oscillation during 2002-2019
Ano2023
MêsJune
Data de Acesso18 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho17476 KiB
2. Contextualização
Autor1 Liu, Xiao
2 Xu, Jiyao
3 Yue, Jia
4 Andrioli, Vania Fátima
Grupo1
2
3
4 DIHPA-CGCE-INPE-MCTI-GOV-BR
Afiliação1 Henan Normal University
2 National Space Science Center
3 Catholic University of America
4 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 xujy@nssc.ac.cn
2
3
4 vania.andrioli@inpe.br
RevistaAtmospheric Chemistry and Physics
Volume23
Número11
Páginas6145-6167
Nota SecundáriaA1_MEDICINA_II A1_INTERDISCIPLINAR A1_GEOCIÊNCIAS A1_ENGENHARIAS_III A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_MATEMÁTICA_/_PROBABILIDADE_E_ESTATÍSTICA A2_ENGENHARIAS_II A2_ASTRONOMIA_/_FÍSICA
Histórico (UTC)2023-06-28 15:52:42 :: simone -> administrator ::
2023-06-28 15:52:43 :: administrator -> simone :: 2023
2023-06-28 15:53:39 :: simone -> administrator :: 2023
2023-12-18 23:44:35 :: administrator -> self-uploading-INPE-MCTI-GOV-BR :: 2023
2023-12-19 02:54:05 :: self-uploading-INPE-MCTI-GOV-BR -> administrator :: 2023
2024-01-02 17:16:44 :: administrator -> simone :: 2023
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoVariations of global wind are important in changing the atmospheric structure and circulation, in coupling of atmospheric layers, and in influencing the wave propagations. Due to the difficulty of directly measuring zonal wind from the stratosphere to the lower thermosphere, we derived a global balance wind (BU) dataset from 50 degrees S to 50 degrees N and during 2002-2019 using the gradient wind theory and SABER temperatures and modified by meteor radar observations at the Equator. The dataset captures the main feature of global monthly mean zonal wind and can be used to study the variations (i.e., annual, semi-annual, ter-annual, and linear) of zonal wind and the responses of zonal wind to quasi-biennial oscillation (QBO), El Nino-Southern Oscillation (ENSO), and solar activity (F-10.7). The same procedure is performed on the MERRA-2 zonal wind (MerU) to validate BU and its responses below 70 km. The annual, semi-annual, and ter-annual oscillations of BU and MerU have similar amplitudes and phases. The semi-annual oscillation of BU has peaks around 80 km, which are stronger in the southern tropical region and coincide with previous satellite observations. As the increasing of the values representing QBO wind, both values of representing BU and MerU (short for BU and MerU) change from increasing to decreasing with the increasing height and extend from the Equator to higher latitudes. Both BU and MerU increase with the increasing of the values of multivariate ENSO index (MEI) and decrease with increasing F-10.7 in the southern stratospheric polar jet region below 70 km. The responses of winds to ENSO and F-10.7 exhibit hemispheric asymmetry and are more significant in the southern polar jet region. While above 70 km, BU increases with the increasing of MEI and F-10.7. The negative linear changes of BU at 50 degrees N are absent in MerU during October-January. The discussions on the possible influences of the temporal intervals and sudden stratospheric warmings (SSWs) on the variations and responses of BU illustrate the following: (1) the seasonal variations and the responses to QBO are almost independent on the temporal intervals selected; (2) the responses to ENSO and F-10.7 are robust but slightly depend on the temporal intervals; (3) the linear changes of both BU and MerU depend strongly on the temporal intervals; (4) SSWs affect the magnitudes but do not affect the hemispheric asymmetry of the variations and responses of BU at least in the monthly mean sense. The variations and responses of global zonal wind to various factors are based on BU, which is derived from observations, and thus provide a good complement to model studies and ground-based observations.
ÁreaCEA
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP3W34T/49C8QJH
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP3W34T/49C8QJH
Idiomaen
Arquivo Alvoacp-23-6145-2023.pdf
Grupo de Usuáriossimone
Visibilidadeshown
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/46KTFK8
Lista de Itens Citandosid.inpe.br/bibdigital/2022/04.03.17.52 2
DivulgaçãoWEBSCI; PORTALCAPES; AGU; SCOPUS.
Acervo Hospedeirourlib.net/www/2021/06.04.03.40
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn keywords lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
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