Resultado da Pesquisa
A expressão de busca foi <firstg dmd and secondaryty pi and y 2010 and dissemination websci>.
20 referências foram encontradas buscando em 17 dentre 17 Arquivos
(este total pode incluir algumas duplicatas - para ver a conta certa clique no botão Mostrar Todas).
As 10 mais recentes estão listadas abaixo.
Data e hora local de busca: 19/04/2024 03:48.

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/37NQTEP
Repositóriodpi.inpe.br/plutao@80/2010/06.25.15.44   (acesso restrito)
Última Atualização2010:08.12.15.48.10 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao@80/2010/06.25.15.44.02
Última Atualização dos Metadados2022:03.08.15.43.08 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1007/s00703-010-0068-x
ISSN0177-7971
Rótulolattes: 9873289111461387 7 NehrkonElWoLiGeLoFr:2010:StTiLa
Chave de CitaçãoNehrkonElWoLiGeLoFr:2010:StTiLa
TítuloCoupled Weather Research and Forecasting - Stochastic Time-Inverted Lagrangian Transport (WRF-STILT) Model
Ano2010
MêsJune
Data de Acesso19 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho911 KiB
2. Contextualização
Autor1 Nehrkon, T.
2 Eluszkiewicz, J.
3 Wofsy, Steven
4 Lin, John
5 Gerbig, C.
6 Longo, Marcos
7 Freitas, Saulo Ribeiro de
Identificador de Curriculo1
2
3
4
5
6
7 8JMKD3MGP5W/3C9JJ7M
Grupo1
2
3
4
5
6
7 DMD-CPT-INPE-MCT-BR
Afiliação1 Atmospher & Environm Res Inc, Lexington, MA USA
2 Harvard Univ, Cambridge, MA 02138 USA
3 Harvard Univ, Cambridge, MA 02138 USA
4 Univ Waterloo, Waterloo, ON N2L 3G1 Canada
5 Max Planck Inst Biogeochem, Jena, Germany
6
7 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 saulo.freitas@cptec.inpe.br
Endereço de e-Mailsaulo.freitas@cptec.inpe.br
RevistaMeteorology and Atmospheric Physics
Volume107
Número1-2
Páginas51-64
Nota SecundáriaB1_GEOCIÊNCIAS B1_INTERDISCIPLINAR
Histórico (UTC)2010-06-29 12:04:21 :: lattes -> marciana :: 2010
2010-07-02 13:12:16 :: marciana -> administrator :: 2010
2010-07-12 17:07:50 :: administrator -> marciana :: 2010
2010-08-12 15:48:10 :: marciana -> administrator :: 2010
2022-03-08 15:43:08 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chaveparticle dispersion model
atmospheric observations
cloud model
system
rams
parameterization
trajectories
emissions
ensemble
fluxes
ResumoThis paper describes the coupling between a mesoscale numerical weather prediction model, the Weather Research and Forecasting (WRF) model, and a Lagrangian Particle Dispersion Model, the Stochastic Time-Inverted Lagrangian Transport (STILT) model. The primary motivation for developing this coupled model has been to reduce transport errors in continental-scale top-down estimates of terrestrial greenhouse gas fluxes. Examples of the model's application are shown here for backward trajectory computations originating at CO2 measurement sites in North America. Owing to its unique features, including meteorological realism and large support base, good mass conservation properties, and a realistic treatment of convection within STILT, the WRF-STILT model offers an attractive tool for a wide range of applications, including inverse flux estimates, flight planning, satellite validation, emergency response and source attribution, air quality, and planetary exploration.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Coupled Weather Research...
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvocouple.pdf
Grupo de Usuáriosadministrator
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marciana
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft12
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
URL (dados não confiáveis)http://www.springerlink.com/content/21h6765l6g426485/fulltext.pdf
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork versiontype
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/38AFL48
Repositóriosid.inpe.br/mtc-m19/2010/09.23.19.22   (acesso restrito)
Última Atualização2015:03.27.17.55.20 (UTC) marciana
Repositório de Metadadossid.inpe.br/mtc-m19/2010/09.23.19.22.15
Última Atualização dos Metadados2021:03.04.03.17.35 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1071/WF08047
ISSN1049-8001
Rótuloself-archiving-INPE-MCTIC-GOV-BR
Chave de CitaçãoCarvalhoJrGASLGRS:2010:UnFiPr
TítuloUnderstorey fire propagation and three mortality on adjacent areas to an Amazonian deforestation fire
Ano2010
Data de Acesso19 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho578 KiB
2. Contextualização
Autor1 Carvalho Jr., João Andrade
2 Gurgel Veras, Carlos Alberto
3 Alvarado, E. C.
4 Sandberg, d. V.
5 Leite, S. J.
6 Gielow, Ralf
7 Rabelo, E. R. C.
8 Santos, José Carlos
Grupo1
2
3
4
5
6 DMD-CPT-INPE-MCT-BR
7
8 LCP-CTE-INPE-MCT-BR
Afiliação1 Universidade Estadual Paulista (UNESP)
2 Universidade de Brasília (UnB)
3 University of Washington
4 USDA Forest Service
5 Universidade do Estado de Mato Grosso (UNEMAT)
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Universidade Estadual Paulista (UNESP)
8 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1
2
3
4
5
6
7
8 jcarlos@lcp.inpe.br
Endereço de e-Mailignes@lcp.inpe.br
RevistaInternational Journal of Wildland Fire
Volume19
Número5
Páginas795-799
Histórico (UTC)2010-12-20 21:58:07 :: ignes@lcp.inpe.br -> marciana :: 2010
2011-09-20 13:30:16 :: marciana -> administrator :: 2010
2018-06-05 04:34:44 :: administrator -> marciana :: 2010
2019-09-23 14:00:03 :: marciana -> administrator :: 2010
2021-03-04 03:17:35 :: administrator -> simone :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chavebiomass combustion
escaped fires
tropical forest
ResumoAbstract Fire characteristics in tropical ecosystems are poorly documented quantitatively in the literature. This paper describes an understorey fire propagating across the edges of a biomass burn of a cleared primary forest. The experiment was carried out in 2001 in the Amazon forest near Alta Floresta, state of Mato Grosso, Brazil, as part of biomass burning experiments conducted in the same area since 1997. The vegetation of a 200 × 200-m2 forested area was clear-cut in early June and burned in late August. The understorey fire that escaped from the main burn was monitored across the four sides of the land clearing area. Flame-front spread varied between 0.14 and 0.35 m min1. Maximum flame height was about 30 cm and typical flame depth was 10 to 15 cm. Tree mortality was investigated in 2003 in four areas adjacent to the biomass burning experiment. A total of 210 trees were counted in the four areas, 29.5% were dead as a consequence of the understorey fire that had occurred 2 years before. This fire-caused mortality is evidence of the synergistic effect between slash burning, tree mortality and future fire vulnerability on the forestland clearing interfaces.
ÁreaCEA
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo Alvocarvalho_understorey.pdf
Grupo de Usuáriosadministrator
ignes@lcp.inpe.br
marciana
Visibilidadeshown
Política de Arquivamentodenypublisher allowfinaldraft
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/3ET38CH
8JMKD3MGPCW/43SKC35
DivulgaçãoWEBSCI
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/37NR2NF
Repositóriodpi.inpe.br/plutao@80/2010/06.25.16.11.46   (acesso restrito)
Última Atualização2010:08.12.13.52.00 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao@80/2010/06.25.16.11.47
Última Atualização dos Metadados2021:01.02.03.52.56 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1007/s00703-009-0050-7
ISSN0177-7971
Rótulolattes: 4336175279058172 2 GomesChan:2010:DePaMo
Chave de CitaçãoGomesChan:2010:DePaMo
TítuloDependence of partitioning of model implicit and explicit precipitation on horizontal resolution
Ano2010
MêsFeb.
Data de Acesso19 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho2283 KiB
2. Contextualização
Autor1 Gomes, Jorge Luís
2 Chan, Chou Sin
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JGRQ
Grupo1 DMD-CPT-INPE-MCT-BR
2 DMD-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 chou@pesquisador.cnpq.br
Endereço de e-Mailchou@pesquisador.cnpq.br
RevistaMeteorology and Atmospheric Physics
Volume106
Número1-2
Páginas1-18
Nota SecundáriaB1_GEOCIÊNCIAS B1_INTERDISCIPLINAR
Histórico (UTC)2010-06-29 12:04:21 :: lattes -> marciana :: 2010
2010-07-02 13:02:35 :: marciana -> administrator :: 2010
2010-07-12 17:13:28 :: administrator -> marciana :: 2010
2010-08-12 13:52:00 :: marciana -> administrator :: 2010
2021-01-02 03:52:56 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveParametrizacao de Convecao Cumulus
Modelo Eta
Microfisica de nuvens
ResumoModel precipitation can be produced implicitly through convective parameterization schemes or explicitly through cloud microphysics schemes. These two precipitation production schemes control the spatial and temporal distribution of precipitation and consequently can yield distinct vertical profiles of heating and moistening in the atmosphere. The partition between implicit and explicit precipitation can be different as the model changes resolutions. Within the range of mesoscale resolutions (about 20 km) and cumulus scale, hybrid solutions are suggested, in which cumulus convection parameterization is acting together with the explicit form of representation. In this work, it is proposed that, as resolution increases, the convective scheme should convert less condensed water into precipitation. Part of the condensed water is made available to the cloud microphysics scheme and another part evaporates. At grid sizes smaller than 3 km, the convective scheme is still active in removing convective instability, but precipitation is produced by cloud microphysics. The Eta model version using KF cumulus parameterization was applied in this study. To evaluate the quantitative precipitation forecast, the Eta model with the KF scheme was used to simulate precipitation associated with the South Atlantic Convergence Zone (SACZ) and Cold Front (CF) events. Integrations with increasing horizontal resolutions were carried out for up to 5 days for the SACZ cases and up to 2 days for the CF cases. The precipitation partition showed that most of precipitation was generated by the implicit scheme. As the grid size decreased, the implicit precipitation increased and the explicit decreased. However, as model horizontal resolution increases, it is expected that precipitation be represented more explicitly. In the KF scheme, the fraction of liquid water or ice, generated by the scheme, which is converted into rain or snow is controlled by a parameter S 1. An additional parameter was introduced into KF scheme and the parameter acts to evaporate a fraction of liquid water or ice left in the model grid by S 1 and return moisture to the resolved scale. An F parameter was introduced to combine the effects of S 1 and S 2 parameters. The F parameter gives a measure of the conversion of cloud liquid water or ice to convective precipitation. A function dependent on the horizontal resolution was introduced into the KF scheme to influence the implicit and explicit precipitation partition. The explicit precipitation increased with model resolution. This function reduced the positive precipitation bias at all thresholds and for the studied weather systems. With increased horizontal resolution, the maximum precipitation area was better positioned and the total precipitation became closer to observations. Skill scores for all events at different forecast ranges showed precipitation forecast improvement with the inclusion of the function F.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > DIDMD > Dependence of partitioning...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
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Arquivo Alvogomes.pdf
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
NotasSetores de Atividade: Pesquisa e desenvolvimento científico.
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage format isbn lineage mark mirrorrepository nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/37NQTCH
Repositóriodpi.inpe.br/plutao@80/2010/06.25.15.43
Última Atualização2010:08.31.17.08.08 (UTC) marciana
Repositório de Metadadosdpi.inpe.br/plutao@80/2010/06.25.15.43.51
Última Atualização dos Metadados2021:01.02.03.52.55 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.5194/acp-10-3505-2010
ISSN1680-7316
Rótulolattes: 9873289111461387 5 TorresChJeAhFrBh:2010:OMMOOb
Chave de CitaçãoTorresChJeAhFrBh:2010:OMMOOb
TítuloOMI and MODIS observations of the anomalous 2008-2009 Southern Hemisphere biomass burning seasons
Ano2010
Data de Acesso19 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho800 KiB
2. Contextualização
Autor1 Torres, O.
2 Chen, Z.
3 Jethva, H.
4 Ahn, C.
5 Freitas, Saulo Ribeiro de
6 Bhartia, P. K.
Identificador de Curriculo1
2
3
4
5 8JMKD3MGP5W/3C9JJ7M
Grupo1
2
3
4
5 DMD-CPT-INPE-MCT-BR
Afiliação1 Dept. of Atmospheric and Planetary Sciences, Hampton University, Hampton, Virginia, USA
2 Dept. of Atmospheric and Planetary Sciences, Hampton University, Hampton, Virginia, USA
3 Dept. of Atmospheric and Planetary Sciences, Hampton University, Hampton, Virginia, USA
4 Science Systems and Applications Inc., Lanham, Maryland, USA
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 4NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
Endereço de e-Mail do Autor1 saulo.freitas@cptec.inpe.br
Endereço de e-Mailsaulo.freitas@cptec.inpe.br
RevistaAtmospheric Chemistry and Physics
Volume10
Número8
Páginas3505-3513
Nota SecundáriaA2_ASTRONOMIA_/_FÍSICA A1_ENGENHARIAS_II A1_GEOCIÊNCIAS A2_INTERDISCIPLINAR
Histórico (UTC)2010-06-29 12:04:21 :: lattes -> marciana :: 2010
2010-08-31 17:08:08 :: marciana -> administrator :: 2010
2010-12-08 15:22:20 :: administrator -> marciana :: 2010
2011-02-24 19:35:32 :: marciana -> administrator :: 2010
2011-02-27 00:14:50 :: administrator -> marciana :: 2010
2011-05-20 05:59:36 :: marciana -> administrator :: 2010
2012-07-25 15:59:10 :: administrator -> marciana :: 2010
2013-02-04 12:58:18 :: marciana -> administrator :: 2010
2021-01-02 03:52:55 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-ChaveAMAZON
DEFORESTATION
VARIABILITY
EMISSIONS
SMOKE
ResumoSignificant inter-annual variability of biomass burning was observed in South America over the 20072009 period. The 2007 number of fires detected from space in South America, as well as the magnitude of the atmospheric aerosol load resulting from fire activity, was the largest over the last ten years. The huge 2007 increase in fire activity was followed by large reductions in the 2008 and 2009 burning seasons. Large drops of the atmospheric load of carbonaceous aerosols over the subcontinent, relative to previous years, was registered in 2008 and 2009 by the OMI sensor onboard the Aura platform, and the MODIS sensors on the Terra and Aqua satellites. The 2009 fire season in South America was the least active of the last ten years. Satellite observations of fire statistics, precipitation, and aerosol optical depth data were used to analyze the fire season over South America and Central Africa during the last ten years to understand the factors that led to the 2007 and 2009 extremes. An analysis of precipitation anomaly data shows that the largest 6-month (MayOctober) precipitation deficit of the last ten years in South America occurred during 2007. The same analysis indicates that in 2009, this region experienced the largest excess precipitation of the decade. Since precipitation is the most important meteorological factor controlling biomass burning activity, it can be concluded that the 2007 maximum and 2009 minimum in fire activity and aerosol load were driven by the observed levels of precipitation. Analysis of the precipitation record, however, does not explain the extremely low 2008 biomass burning activity. Although the 2008 precipitation deficit was similar in magnitude to the one that in 2005 contributed to the second Correspondence to: O. Torres (omar.torres@hamptonu.edu) most intense biomass burning season in the last ten years, the 2008 fire season was surprisingly weak. The combined analysis of satellite data on atmospheric aerosol load, fire counts and precipitation strongly suggests that the observed 2008 decline in aerosol load and fire activity in South America was heavily influenced by conditions other than meteorological factors.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > OMI and MODIS...
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URL dos dadoshttp://urlib.net/ibi/J8LNKAN8RW/37NQTCH
URL dos dados zipadoshttp://urlib.net/zip/J8LNKAN8RW/37NQTCH
Idiomaen
Arquivo AlvoFreitas_OMI.pdf
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Política de Arquivamentoallowpublisher allowfinaldraft
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
URL (dados não confiáveis)http://www.atmos-chem-phys.net/10/3505/2010/acp-10-3505-2010.html
DivulgaçãoWEBSCI; PORTALCAPES; AGU.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/36KNR5L
Repositóriodpi.inpe.br/plutao@80/2009/12.22.15.39   (acesso restrito)
Última Atualização2010:04.16.12.24.04 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao@80/2009/12.22.15.39.02
Última Atualização dos Metadados2021:01.02.03.52.54 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1002/asl.246
ISSN1530-261X
Rótulolattes: 4524628383146981 1 LimaSaty:2009:PoHeRa
Chave de CitaçãoLimaSaty:2010:PoHeRa
TítuloPost-summer heavy rainfall events in Southeast Brazil associated with South Atlantic Convergence Zone
Ano2010
Mêsjan-mar
Data de Acesso19 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho2218 KiB
2. Contextualização
Autor1 Lima, Kellen Carla
2 Satyamurty, Prakki
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JJ4J
Grupo1 DMD-CPT-INPE-MCT-BR
2 DMD-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 kellen.lima@cptec.inpe.br
Endereço de e-Mailkellen.lima@cptec.inpe.br
RevistaAtmospheric Science Letters
Volume11
Número1
Páginas13-20
Nota SecundáriaB3_ENGENHARIAS_I B3_GEOCIÊNCIAS
Histórico (UTC)2009-12-23 14:00:51 :: lattes -> marciana ::
2010-04-16 12:24:04 :: marciana -> administrator ::
2010-05-12 02:06:58 :: administrator -> marciana ::
2010-07-16 15:49:56 :: marciana -> administrator ::
2021-01-02 03:52:54 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chaveextreme precipitation events
patterns
America
ResumoHeavy rainfall events (HREs) in the post-summer month of March in Southeast Brazil cause disasters such as floods, mudslides and landslides, mainly because the soil becomes saturated by February. Forty-five years of rainfall data show that heavy rainfall frequency increases again in the month of March. The composite anomaly fields of the atmospheric circulation during and before HREs associated with the formation of South Atlantic Convergence Zone show some special characteristics that may be used as a guide for early warning. The convergence of moisture flux in the troposphere over the region grows 40% during the 48 h before the HRE in March. Copyright (C) 2010 Royal Meteorological Society.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Post-summer heavy rainfall...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvoprakki_post.pdf
Grupo de Usuáriosadministrator
lattes
marciana
Grupo de Leitoresadministrator
marciana
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.58.28 1
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/36KNNB5
Repositóriodpi.inpe.br/plutao@80/2009/12.22.15.05
Última Atualização2010:08.31.17.01.32 (UTC) marciana
Repositório de Metadadosdpi.inpe.br/plutao@80/2009/12.22.15.05.03
Última Atualização dos Metadados2021:01.02.03.52.54 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.5194/acp-10-4977-2010
ISSN1680-7316
Rótulolattes: 9873289111461387 6 MarecalPiRiPoCrFrLo:2009:MoReUp
Chave de CitaçãoMarecalPiRiPoCrFrLo:2010:MoReUp
TítuloModelling the reversible uptake of chemical species in the gas phase by ice particles formed in a convective cloud
Ano2010
Data de Acesso19 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1560 KiB
2. Contextualização
Autor1 Marecal, V
2 Pirre, M
3 Riviere, E D
4 Pouvesle, N.
5 Crowley, J. N.
6 Freitas, Saulo Ribeiro de
7 Longo, K. M.
Identificador de Curriculo1
2
3
4
5
6
7
8
9
10
11 8JMKD3MGP5W/3C9JJ7M
Grupo1
2
3
4
5
6 DMD-CPT-INPE-MCT-BR
7 DGE-CEA-INPE-MCT-BR
Afiliação1 1Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS-Universit´e d’Orl´eans, UMR6115, Orl´eans, France
2 1Laboratoire de Physique et Chimie de l’Environnement et de l’Espace, CNRS-Universit´e d’Orl´eans, UMR6115, Orl´eans, France
3 Groupe de Spectrom´etrie Mol´eculaire et Atmosph´erique, Universit´e de Reims-CNRS, Reims, France
4 Max-Planck-Institut f¨ur Chemie, Division of Atmospheric Chemistry, Mainz, Germany
5 Max-Planck-Institut f¨ur Chemie, Division of Atmospheric Chemistry, Mainz, Germany
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1
2
3
4
5
6 saulo.freitas@cptec.inpe.br
Endereço de e-Mailsaulo.freitas@cptec.inpe.br
RevistaAtmospheric Chemistry and Physics
Volume10
Número10
Páginas4977–5000
Nota SecundáriaB4_ENGENHARIAS_II B3_GEOCIÊNCIAS B2_INTERDISCIPLINAR
Histórico (UTC)2009-12-23 14:00:48 :: lattes -> marciana ::
2010-01-06 11:54:49 :: marciana -> administrator ::
2010-01-26 15:36:58 :: administrator -> banon ::
2010-05-11 16:35:19 :: banon -> administrator ::
2010-05-12 02:06:45 :: administrator -> marciana ::
2010-08-31 17:01:32 :: marciana -> administrator :: 2009 -> 2010
2010-12-08 15:19:42 :: administrator -> marciana :: 2010
2011-02-24 19:07:04 :: marciana -> administrator :: 2010
2011-02-27 00:14:49 :: administrator -> marciana :: 2010
2011-05-20 05:50:06 :: marciana -> administrator :: 2010
2012-07-25 15:58:10 :: administrator -> marciana :: 2010
2013-02-04 12:15:35 :: marciana -> administrator :: 2010
2021-01-02 03:52:54 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoThe present paper is a preliminary study preparing the introduction of reversible trace gas uptake by ice particles into a 3-D cloud resolving model. For this a 3-D simulation of a tropical deep convection cloud was run with the BRAMS cloud resolving model using a two-moment bulk microphysical parameterization. Trajectories within the convective clouds were computed from these simulation outputs along which the variations of the pristine ice, snow and aggregate mixing ratios and concentrations were extracted. The reversible uptake of 11 trace gases by ice was examined assuming applicability of Langmuir isotherms using recently evaluated (IUPAC) laboratory data. The results show that ice uptake is only significant for HNO3, HCl, CH3COOH and HCOOH. For H2O2, using new results for the partition coefficient results in significant partitioning to the ice phase for this trace gas also. It was also shown that the uptake is largely dependent on the temperature for some species. The adsorption saturation at the ice surface for large gas mixing ratios is generally not a limiting factor except for HNO3 and HCl for gas mixing ratio greater than 1 ppbv. For HNO3, results were also obtained using a trapping theory, resulting in a similar order of magnitude of uptake, although the two approaches are based on different assumptions. The results were compared to those obtained using a BRAMS cloud simulation based on a single-moment microphysical scheme instead of the two moment scheme. We found similar results with a slightly more important uptake when using the singlemoment scheme which is related to slightly higher ice mixing ratios in this simulation. The way to introduce these results in the 3-D cloud model is discussed.
ÁreaMET
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/J8LNKAN8RW/36KNNB5
URL dos dados zipadoshttp://urlib.net/zip/J8LNKAN8RW/36KNNB5
Idiomaen
Arquivo AlvoFreitas_Modelling.pdf
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EU29DP
8JMKD3MGPCW/43SKC35
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.01.22.11 1
URL (dados não confiáveis)http://www.atmos-chem-phys-discuss.net/9/24361/2009/acpd-9-24361-2009.html
DivulgaçãoWEBSCI; PORTALCAPES; AGU.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn keywords lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/37SMPN8
Repositóriosid.inpe.br/mtc-m19@80/2010/07.19.13.04   (acesso restrito)
Última Atualização2015:03.26.14.03.22 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m19@80/2010/07.19.13.04.58
Última Atualização dos Metadados2021:01.02.03.52.31 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1007/s00704-010-0270-2
ISSN0177-798X
Chave de CitaçãoSansigoloKaya:2010:TrSeMa
TítuloTrends of seasonal maximum and minimum temperatures and precipitation in Southern Brazil for the 1913-2006 period
Ano2010
Data de Acesso19 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho6429 KiB
2. Contextualização
Autor1 Sansigolo, Clóvis Angeli
2 Kayano, Mary Toshie
Grupo1 DMD-CPT-INPE-MCT-BR
2 DMD-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 clovis.sansigolo@cptec.inpe.br
2 mary.kayano@cptec.inpe.br
RevistaTheoretical and Applied Climatology
Volume101
Número1-2
Páginas209 - 216
Nota SecundáriaB2_ASTRONOMIA_/_FÍSICA A2_CIÊNCIAS_AGRÁRIAS_I B1_GEOCIÊNCIAS A2_GEOGRAFIA A2_INTERDISCIPLINAR
Histórico (UTC)2011-05-24 23:17:48 :: marciana -> administrator :: 2010
2012-11-21 14:56:17 :: administrator -> marciana :: 2010
2013-02-22 14:57:27 :: marciana -> administrator :: 2010
2021-01-02 03:52:31 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chaveextremes
america
ResumoLong-term variations of monthly average maximum and minimum temperature (TMAX and TMIN) and precipitation records in southern Brazil are investigated for the 1913-2006 period. These variations are carefully analyzed for seasonal and annual indices, taken as regional averages. For this purpose, the serial correlation and trend of the indices are investigated using the run and Mann-Kendall tests. The significant trends are obtained from linear least-square fits. The annual and seasonal TMIN indices show significant warming trends with magnitudes (1.7A degrees C per 100 years for annual index) comparable to those reported by the Intergovernmental Panel on Climate Change, but lower than those found for the southern Brazil in another previous work. Regarding the two other variables, the indices show significant trends only for summer, being a cooling trend of 0.6A degrees C per 100 years for the TMAX and an increasing trend of 93 mm per 100 years over an average summer precipitation of 367 mm. Concerning the decadal analysis, the 1920s present the lowest annual, autumn, and spring TMIN and the 1990s, the highest ones. The 1970s is the decade with the lowest summer TMAX, and the 1940s the decade with the highest one. The driest decade is the 1940s and the wettest, the 1980s.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Trends of seasonal...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
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4. Condições de acesso e uso
Idiomaen
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Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft12
Permissão de Leituradeny from all and allow from 150.163
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5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate session shorttitle sponsor subject targetfile tertiarymark tertiarytype url
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/37SMMTB
Repositóriosid.inpe.br/mtc-m19@80/2010/07.19.12.42
Última Atualização2013:04.15.14.42.34 (UTC) marciana
Repositório de Metadadossid.inpe.br/mtc-m19@80/2010/07.19.12.42.29
Última Atualização dos Metadados2021:01.02.03.52.31 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1175/2010JPO4349.1
ISSN0022-3670
Chave de CitaçãoInnocentiniGonç:2010:ImSpDr
TítuloThe Impact of spume droplets and wave stress parameterizations on simulated near-surface maritime wind and temperature
ProjetoFAPESP (2005/59438-9; 2008/58595-1)
Ano2010
MêsJune
Data de Acesso19 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho824 KiB
2. Contextualização
Autor1 Innocentini, Valdir
2 Gonçalves, Iury Angelo
Grupo1 DMD-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 valdir@cptec.inpe.br
RevistaJournal of Physical Oceanography
Volume40
Número6
Páginas1373 - 1389
Nota SecundáriaA2_GEOCIÊNCIAS
Histórico (UTC)2011-05-22 13:43:52 :: marciana -> administrator :: 2010
2013-03-11 18:39:47 :: administrator -> marciana :: 2010
2013-04-15 14:42:34 :: marciana -> administrator :: 2010
2021-01-02 03:52:31 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chavesea-surface
air-flow
spray
generation
height
layer
water
drag
prediction
intensity
ResumoThe influence of ocean gravity waves on the wind and temperature above the surface is investigated using a one-dimensional boundary layer model. The effect of the wave-induced stress is evaluated using three parameterizations: wave age (WaAg), wave steepness (WaSt), and wind action on the wave spectrum (WiAc). It is found that while the WaAg is more effective in reducing the wind for young waves, in the WaSt approach the maximum reduction is for old waves. On the other hand, the WiAc is very sensitive to the energy present in high frequencies corresponding to periods less than 2 s, which are found in both young and mature spectra. Since observations show that most of the wave stress is due to the small-period wave energy, in this aspect the WaSt parameterization is not recommended; WaAg is not as accurate; and thus WiAc is the best among the three, although its computational cost is the highest. The droplet load contribution to the total surface stress can be neglected for the droplet spectrum produced by 10-m wind speeds up to 15 m s(-1), but its importance increases with the speed and its magnitude becomes about 1/5 of the total stress for wind speed similar to 30 m s(-1). Concerning the latent and sensible heat fluxes accompanying the production of spume droplets by waves, a feasible microphysical formulation for operational use in weather forecasting models is proposed. The droplet spectrum is assumed to be a product of two functions, one depending on the windsea Reynolds number and the other on the droplet radius spectrum. The bulk effect of the latter is analytically evaluated and stored in a table as a function of air temperature T-a, relative humidity R-%, and significant wave height H-s. In numerical experiments with initial sea surface temperature 5 K higher than the air surface, latent and sensible heat contributions to the air temperature are computed as a function of the wave spectra. The launched droplet spectrum (which increases the air temperature due to sensible heat) and the relative humidity (which controls the cooling due to the droplet evaporation) define the heat budget and the air temperature evolution. Although in these experiments the sea temperature is much higher than the air temperature, the results show a noticeable dominance of the evaporative cooling in the lower atmosphere mainly for smaller significant wave height. Some air warming is noticeable only from a threshold around H-s >= 5 m.
ÁreaMET
Arranjourlib.net > DIDMD > The Impact of...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP7W/37SMMTB
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP7W/37SMMTB
Idiomaen
Arquivo Alvo2010jpo4349.1.pdf
Grupo de Usuáriosmarciana
Grupo de Leitoresadministrator
marciana
Visibilidadeshown
Política de Arquivamentodenypublisher6 allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress readpermission resumeid rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/37BAREE
Repositóriosid.inpe.br/mtc-m19@80/2010/04.15.18.56   (acesso restrito)
Última Atualização2010:04.15.19.02.41 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m19@80/2010/04.15.18.56.40
Última Atualização dos Metadados2021:01.02.03.52.30 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1002/asl.247
ISSN1530-261X
Chave de CitaçãoVasconcellosCava:2010:ExPrOv
TítuloExtreme precipitation over Southeastern Brazil in the austral summer and relations with the Southern Hemisphere annular mode
Ano2010
Mêsjan.-mar.
Data de Acesso19 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho936 KiB
2. Contextualização
Autor1 Vasconcellos, Fernanda Cerqueira
2 Cavalcanti, Iracema Fonseca de Albuquerque
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHDE
Grupo1 DMD-CPT-INPE-MCT-BR
2 DMD-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Maildeicy.farabello@cptec.inpe.br
RevistaAtmospheric Science Letters
Volume11
Número1
Páginas21-26
Nota SecundáriaB1_GEOCIÊNCIAS
Histórico (UTC)2010-04-15 19:02:41 :: deicy -> administrator ::
2010-05-11 01:00:34 :: administrator -> deicy ::
2010-07-05 14:56:50 :: deicy -> marciana ::
2011-05-24 23:28:23 :: marciana -> administrator :: 2010
2021-01-02 03:52:30 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chaveatlantic convergence zone
sea surface temperature
South America
climate change
precipitation events
Argentina
variability
circulation
Brazil
ResumoSoutheastern Brazil is a highly industrialized and populated region which largely contributes to the country's economy. Extreme precipitation over this region can cause floods and landslides occurrences or lack of precipitation that can affect many sectors of economy. The objective of this work is to identify atmospheric characteristics associated with austral summer extreme precipitation over part of Southeastern Brazil. The atmospheric characteristics obtained from wet and dry composites suggest that extreme precipitation was associated with anomalous circulation over the region, forced by a PSA-like wavetrain intensified by the Southern Annular Mode. Copyright (C) 2010 Royal Meteorological Society.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Extreme precipitation over...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo AlvoCavalcanti_extreme.pdf
Grupo de Usuáriosadministrator
deicy
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage electronicmailaddress format isbn label lineage mark nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/37B5QSE
Repositóriosid.inpe.br/mtc-m19@80/2010/04.14.15.29   (acesso restrito)
Última Atualização2010:04.14.15.32.41 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m19@80/2010/04.14.15.29.16
Última Atualização dos Metadados2021:01.02.03.52.29 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1007/s00704-009-0107-z
ISSN0177-798X
Chave de CitaçãoGarciaKaya:2010:SoEvRe
TítuloSome evidence on the relationship between the South American monsoon and the Atlantic ITCZ
Ano2010
Mêsjan
Data de Acesso19 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho809 KiB
2. Contextualização
Autor1 Garcia, Samia R.
2 Kayano, Mary T
Grupo1 DMD-CPT-INPE-MCT-BR
2 DMD-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Maildeicy.farabello@cptec.inpe.br
RevistaTheoretical and Applied Climatology
Volume99
Número1-2
Páginas29-38
Nota SecundáriaA2_CIÊNCIAS_AGRÁRIAS A2_GEOCIÊNCIAS A2_GEOGRAFIA A2_INTERDISCIPLINAR
Histórico (UTC)2010-04-14 15:32:41 :: deicy -> administrator ::
2010-05-11 01:00:33 :: administrator -> deicy ::
2010-07-05 14:56:50 :: deicy -> administrator ::
2021-01-02 03:52:29 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chaveannual cycle
hemisphere
rainfall
ResumoThe seasonal variations of convection associated with the South American monsoon system (SAMS) are analyzed using pentad means of outgoing longwave radiation (OLR) data during the 1979-2006 period. The data is filtered for the 0.4-1.2 year scale and an empirical orthogonal function (EOF) analysis is applied. The results provide three dominant modes with distinct convective features, which are referred to as: equatorially antisymmetric, intertropical convergence zone (ITCZ) and symmetric modes. The first two modes vary in an annual scale, and the latter one in a semiannual scale. The evolving aspects of these modes are studied by correlating (lagged and simultaneously) the principal component of each mode and the filtered OLR time series. The antisymmetric and the ITCZ modes evolve smoothly into each other reflecting the northwestward and northeastward propagation of convective activity. The propagation rates vary depending on development stage and region considered. On the other hand, the symmetric mode with the largest convective activity in the western Amazon evolves independently, and depicts the transition from dry to wet seasons and vice-versa.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Some evidence on...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo AlvoSamia_Some Evidence.pdf
Grupo de Usuáriosadministrator
deicy
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft12
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
DivulgaçãoWEBSCI; PORTALCAPES; MGA.
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage electronicmailaddress format isbn label lineage mark nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
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