Resultado da Pesquisa
A expressão de busca foi <firstg dsa and secondaryty pi and y 2004 and (dissemination websci or dissemination portalcapes)>.
7 referências encontradas buscando em 17 dentre 17 Arquivos.
Data e hora local de busca: 26/04/2024 20:02.
1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificadorx6e6X3pFwXQZ3DUS8rS5/CMf3u
Repositóriocptec.inpe.br/walmeida/2004/07.16.14.47   (acesso restrito)
Última Atualização2004:12.08.02.00.00 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/walmeida/2004/07.16.14.47.44
Última Atualização dos Metadados2022:03.26.18.00.05 (UTC) administrator
Chave SecundáriaINPE-11144-PRE/6600
ISSN0177-798X
Chave de CitaçãoFischTMSLNDG:2004:CoBoLa
TítuloThe convective boundary layer over pasture and forest in Amazonia
Ano2004
MêsJun.
Data de Acesso26 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho426 KiB
2. Contextualização
Autor1 Fisch, Gilberto
2 Tota, Julio
3 Machado, Luis Augusto Toledo
4 Silva Dias, Maria Assuncao Faus da
5 Lyra, R. F. D.
6 Nobre, Carlos Afonso
7 Dolman, A. J.
8 Gash, J. H. C .
Identificador de Curriculo1
2
3
4
5
6 8JMKD3MGP5W/3C9JGQ7
Grupo1 DSA-INPE-MCT-BR
2 CG-INPE-MCT-BR
3 DMA-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
Endereço de e-Mailfabia@cptec.inpe.br
RevistaTheoretical and Applied Climatology
Volume78
Número1-3
Páginas47-59
Histórico (UTC)2004-12-08 12:29:12 :: Fabia -> administrator ::
2008-06-10 19:50:39 :: administrator -> estagiario ::
2010-05-11 16:54:04 :: estagiario -> administrator ::
2022-03-26 18:00:05 :: administrator -> marciana :: 2004
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chavedeforestation
growth
model
ResumoThe coupling between different types of surface (tropical forest or grass) and the Convective Boundary Layer (CBL) has been investigated using observational (rawinsoundings) data collected over Rondônia in southwest Amazonia. The data reported here support the notion that deforestation may modify the dynamics of the boundary layer, in particular during the dry season. In this period the sensible heat fluxes are very high over pasture, creating a CBL around 550m deeper compared to that over the forest. The measurements showed the height of the fully developed CBL for pasture to be 1650m, compared to around 1100m for forest. During the wet season the height of the CBL is lower than during the dry season and has the same height (around 1000m) for forest and pasture sites. The CBL over pasture is hotter and drier than over forest during the dry season, but during the wet season the air temperatures and humidities are similar. Comparing the CBL growth during the dry and wet season, there is evidence that the CBL properties over the forest are not dependent on the surface characteristics, but over the pasture they are.
ÁreaMET
Arranjo 1urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > The convective boundary...
Arranjo 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > The convective boundary...
Arranjo 3urlib.net > BDMCI > Fonds > Produção até 2016 > DMA > The convective boundary...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo AlvoFisch_The convective boundary.pdf
Grupo de UsuáriosFabia
administrator
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentodenypublisher denyfinaldraft12
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
8JMKD3MGPCW/43SRC6S
8JMKD3MGPCW/46JKC45
URL (dados não confiáveis)http://www.springerlink.com/app/home/contribution.asp?wasp=6cclymvhlm5jf40wmj13&referrer=parent&backto=issue,5,14;journal,2,38;linkingpublicationresults,1:101580,1
DivulgaçãoWEBSCI; PORTALCAPES; MGA.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarymark 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-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificadorx6e6X3pFwXQZ3DUS8rS5/BQPSi
Repositóriocptec.inpe.br/walmeida/2004/04.22.13.30
Última Atualização2004:10.29.03.00.00 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/walmeida/2004/04.22.13.30.50
Última Atualização dos Metadados2021:02.10.23.11.27 (UTC) administrator
Chave SecundáriaINPE-10641-PRE/6103
ISSN0027-0644
Chave de CitaçãoMachadoLaur:2004:CoSyAr
TítuloThe convective system area expansion over Amazonia and its relationships with convective system life duration and high-level wind divergence
Ano2004
Mêsmar
Data de Acesso26 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho997 KiB
2. Contextualização
Autor1 Machado, Luiz Augusto Toledo
2 Laurent, H.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JHMS
Grupo1 DSA-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cahoeira Paulista- 12630000-SP- BRAZIL
Endereço de e-Mailfabia@cptec.inpe.br
RevistaMonthly Weather Review
Volume132
Número3
Páginas714-725
Histórico (UTC)2004-10-29 13:06:06 :: Fabia -> administrator ::
2008-06-10 19:50:12 :: administrator -> estagiario ::
2010-05-11 16:53:00 :: estagiario -> administrator ::
2021-02-10 23:11:27 :: administrator -> marciana :: 2004
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chaveradar
cycle
WETAMC/LBA
satellite
fields
cloud
ResumoThe relationships between the initial area expansion rate of tropical convective systems and their total life duration are analyzed during the period of the Wet Season Amazon Mesoscale Campaign/Large-Scale Biosphere Atmosphere (WETAMC/LBA) experiment over tropical South America, using an objective tracking of convective systems during their life cycle from infrared Geostationary Operational Environmental Satellite (GOES) images. The results show that it is possible to estimate the probable lifetime of a convective system, within certain error bars, considering only its initial area expansion. This result shows that the initial area expansion could be used as a predictor of the life cycle of convective systems. The area expansion is also a good indicator of convective activity such as the diurnal cycle of convection. Over the southwest Amazon, the maximum area expansion occurs close to the time of maximum precipitation and about 4 h before the maximum cold cloud fraction at the same threshold (235 K). Also, the hypothesis that the area expansion, and hence the convective activity, impacts the high-level wind divergence has been investigated using satellite wind observations. It is found that the wind divergence fields derived are able to describe the large-scale patterns but are not able to capture the small-scale features. The diurnal cycle of the high-level wind divergence generally shows a flat response over tropical South America, although a coherent but not significant signal is observed over the WETAMC/LBA area. It is shown that the area of the cloud shield of convective systems varies not only in association with the upper-level wind divergence but also with the condensation-evaporation process. The increase of area in this initial stage is mainly due to the condensation process. During the ensuing mature stage, the upper-air wind divergence also contributes to the expansion.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > The convective system...
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/x6e6X3pFwXQZ3DUS8rS5/BQPSi
URL dos dados zipadoshttp://urlib.net/zip/x6e6X3pFwXQZ3DUS8rS5/BQPSi
Idiomaen
Arquivo AlvoMWR2004_pub.pdf
Grupo de Usuáriosadministrator
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentodenypublisher6 allowfinaldraft
Permissão de Leituraallow from all
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 1
DivulgaçãoWEBSCI; PORTALCAPES; MGA.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository 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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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificadorx6e6X3pFwXQZ3DUS8rS5/Es9ye
Repositóriocptec.inpe.br/walmeida/2004/12.13.08.24
Última Atualização2018:02.27.14.17.06 (UTC) marciana
Repositório de Metadadoscptec.inpe.br/walmeida/2004/12.13.08.24.01
Última Atualização dos Metadados2021:02.10.23.11.32 (UTC) administrator
Chave SecundáriaINPE-11884-PRE/7231
ISSN0003-0007
Rótuloself-archiving-INPE-MCTIC-GOV-BR
Chave de CitaçãoMachadoLaur:2004:NeMeEv
TítuloNew method to evaluate cloud seeding
Ano2004
Mêsapr.
Data de Acesso26 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho155 KiB
2. Contextualização
Autor1 Machado, Luis Augusto Toledo
2 Laurent, H.
Grupo1 DSA-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
Endereço de e-Mailatus@cptec.inpe.br
RevistaBulletin of the American Meteorological Society
Volume85
Número4
Páginas492-495
Histórico (UTC)2005-01-13 10:47:50 :: fabia -> administrator ::
2008-06-10 19:51:30 :: administrator -> estagiario ::
2010-05-11 16:55:33 :: estagiario -> administrator ::
2013-03-06 19:18:50 :: administrator -> marciana :: 2004
2018-02-27 14:17:07 :: marciana -> administrator :: 2004
2021-02-10 23:11:32 :: administrator -> marciana :: 2004
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoA new method for the objective evaluation of short-term, nonrandomized, operational, convective cloud-seeding projects on a floating- target area basis was used to evaluate seeding effects in the Texas High Plains (HP) and Edwards Aquifer (EA) programs during the 1999,2000, and 2001 (EA only) seasons Seeded and matching control units were defined in accordance with unit definition in previous randomized seeding in Texas and Thailand. The units were defined and selected by a computerized automatic algorithm, which is not subject to human bias.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > New method to...
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/x6e6X3pFwXQZ3DUS8rS5/Es9ye
URL dos dados zipadoshttp://urlib.net/zip/x6e6X3pFwXQZ3DUS8rS5/Es9ye
Idiomaen
Arquivo Alvo11884.pdf
Grupo de Usuáriosadministrator
fabia
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentodenypublisher6 allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 2
DivulgaçãoWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Notascomments
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel doi electronicmailaddress format isbn keywords lineage mark mirrorrepository nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarymark 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-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificadorx6e6X3pFwXQZ3DUS8rS5/BRtbG
Repositóriocptec.inpe.br/walmeida/2004/04.23.14.40   (acesso restrito)
Última Atualização2004:12.07.02.00.00 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/walmeida/2004/04.23.14.40.41
Última Atualização dos Metadados2021:02.10.23.11.29 (UTC) administrator
Chave SecundáriaINPE-10640-PRE/6102
ISSN0177-798X
Chave de CitaçãoMachadoLaurDessMira:2004:CoDiVe
TítuloSeasonal and diurnal variability of convection over the Amazonia: A comparison of different vegetation types and large scale forcing
Ano2004
Mêsapr
Data de Acesso26 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho687 KiB
2. Contextualização
Autor1 Machado, Luiz Augusto Toledo
2 Laurent, H.
3 Dessay, N.
4 Miranda, I.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JHMS
Grupo1 DSA-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cachoeira Paulista -12630000-SP-Brasil
Endereço de e-Mailfabia@cptec.inpe.br
RevistaTheoretical and Applied Climatology
VolumeOnline First
NúmeroDOI: 10.1007/s00704-004-0044-9
Histórico (UTC)2004-12-07 15:27:16 :: Fabia -> administrator ::
2006-11-17 23:11:17 :: administrator -> estagiario ::
2010-05-11 16:53:01 :: estagiario -> administrator ::
2021-02-10 23:11:29 :: administrator -> marciana :: 2004
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chaveclimatogical
ResumoA climatological description of the convection over Amazonia is based on the seasonal and diurnal cycle analysis. Long series of observations are used from four sites: two sites are representative of dense rainforest, either continental (Manaus) or coastal (Belém); one site is in southeast Amazonia, in a region of ecological tension where forest has been partly replaced by pasture (Vilhena); and finally, one is in the south of Amazonia, in a region typical of savanna (Brasília). Each site has a long series of radiosonde and surface observations. Other parameters are also used: rainfall averaged from the raingauges in the vicinity of each site; vegetation monitored using NDVI averaged over 128km×128km boxes centred on each site; and total and high cloud cover estimated using the 2.5°×2.5° ISCCP products derived from satellite data. It is shown that the main differences between rainforest and savanna or deforested sites occur in the dry season, whereas the magnitude and diurnal cycle of convection as well as amount of rainfall and NDVI are quite similar during the wet season. For the savanna site the seasonal variation is well defined for every parameter, whereas for rainforest sites the vegetation and atmospheric thermodynamics show very weak seasonal variations, yet driving significant diurnal variations of the convection and precipitation. The transition season from dry to wet and the beginning of the wet season is generally the period of strongest intensity of convection.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > Seasonal and diurnal...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo AlvoMachado_Seasonal and diurnal.pdf
Grupo de Usuáriosadministrator
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentodenypublisher denyfinaldraft12
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
URL (dados não confiáveis)http://www.springerlink.com/media/H0XF475FNB1JPNAA2W97/Contributions/E/9/Y/9/E9Y91XUGN6R8CXQH.pdf
DivulgaçãoWEBSCI; PORTALCAPES; MGA.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid pages parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork versiontype
7. Controle da descrição
e-Mail (login)marciana
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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
Identificadorx6e6X3pFwXQZ3DUS8rS5/EcD6E
Repositóriocptec.inpe.br/walmeida/2004/11.18.10.19   (acesso restrito)
Última Atualização2004:11.18.02.00.00 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/walmeida/2004/11.18.10.19.23
Última Atualização dos Metadados2021:02.10.23.11.32 (UTC) administrator
Chave SecundáriaINPE-11684-PRE/7043
ISSN0169-8095
Chave de CitaçãoPlana-FattoriDubuFomiCorr:2004:EsAtWa
TítuloEstimating the atmospheric water vapor content from multi-filter rotating shadow-band radiometry at Sao Paulo, Brazil
Ano2004
Mêsaug./set.
Data de Acesso26 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho613 KiB
2. Contextualização
Autor1 Plana-Fattori, Artemio
2 Dubuisson, Philippe
3 Fomin, Boris Alexeevitch
4 Correa, Marcelo de Paula
Grupo1 DSA-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
Endereço de e-Mailatus@cptec.inpe.br.
RevistaAtmospheric Research
Volume71
Número3
Páginas171-192
Histórico (UTC)2004-12-06 11:18:22 :: fabia -> administrator ::
2008-06-10 19:51:21 :: administrator -> estagiario ::
2010-05-11 16:55:23 :: estagiario -> administrator ::
2021-02-10 23:11:32 :: administrator -> marciana :: 2004
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chavesolar transmission measurements
near-infrared
atmospheric water vapor content
aerosol optical depth
atmospheric turbidity
Sao Paulo
Brazil
molecular spectroscopic database
sun photometer
differential absorption
precipitable water
optical dept
trace gases
solar
aerosol
radiation
instrument
ResumoSelected measurements performed with Multi-Filter Rotating Shadow-band Radiometers under cloudless conditions at an urban tropical site, Sao Paulo, Brazil (23.65degreesS, 46.62degreesW, 800 m above the mean sea level) are analyzed. Water vapor content (U) values are estimated from the analysis of measurements performed near 940 run with two bandwidths (10 and 3 5 nm). Narrow- and wide-band measurements performed near 940 nm are analyzed separately with the help of line-by-line radiative model computed transmittances, allowing independent (U) over cap (N) and (U) over cap (W) estimates. The ratio of these measurements is also analyzed, allowing a third water vapor content estimate (<(U) over cap>(NW)). Selected approaches for computing water vapor absorption are compared, including two line parameter databases and two line-by-line models. After pooling, all results obtained from measurements performed during 16 cloudless mornings and representing the water vapor absorption through HITRAN-2000 line parameters and CKD-2.4 continuum model, estimates (U) over cap (N), (U) over cap (W), and (U) over cap (NW) were on average 1.8, 0.5, and 4.0 kg m(-2) lower than respective values provided by balloon-borne soundings, respectively; and (4, estimates were 3% to 14% smaller than respective (U) over cap (W) values. Assuming that the independent values provided by soundings are accurate, the ad hoc reduction of continuum absorption coefficients to 50% of values provided by CKD-2.4 model improved the reliability of narrow-band water vapor content estimates in this study. Lastly, the influence of aerosol extinction on water vapor content was minimized from the analysis of measurements performed near 870 and 1035 nm. The corresponding turbidity exponent a assumed values between 0.7 and 1.1, which is somewhat weaker than those usually reported for urban conditions. (C) 2004 Elsevier B.V. All rights reserved.
ÁreaMET
Arranjourlib.net > DIDSA > Estimating the atmospheric...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo AlvoPlana-Fattori_Estimating_.pdf
Grupo de Usuáriosadministrator
fabia
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/43SRC6S
DivulgaçãoWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
e-Mail (login)marciana
atualizar 

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificadorx6e6X3pFwXQZ3DUS8rS5/BGDdi
Repositóriocptec.inpe.br/walmeida/2004/04.08.10.18
Última Atualização2004:11.26.02.00.00 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/walmeida/2004/04.08.10.18.20
Última Atualização dos Metadados2021:02.10.23.11.26 (UTC) administrator
Chave SecundáriaINPE-10646-PRE/6108
ISSN0894-8755
Chave de CitaçãoSiqueiraMach:2004:InFrSy
TítuloInfluence of the Frontal Systems on the Day-to-Day Convection Variability over South America
Ano2004
Mêsmay
Data de Acesso26 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1290 KiB
2. Contextualização
Autor1 Siqueira, Jose Ricardo
2 Machado, Luiz Augusto Toledo
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHMS
Grupo1 DSA-INPE-MCT-BR
Afiliação1 CPTEC-INPE- Sao Jose dos Campos-SP-Brazil
Endereço de e-Maildeicy@cptec.inpe.br
RevistaJournal of Climate
Volume17
Número9
Páginas1754 - 1766
Histórico (UTC)2004-11-26 11:41:41 :: Deicy -> administrator ::
2012-11-20 04:06:18 :: administrator -> Deicy :: 2004
2013-02-20 14:52:33 :: Deicy -> administrator :: 2004
2021-02-10 23:11:26 :: administrator -> marciana :: 2004
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveAmazon basin
climatology
ResumoCold cloud-top fractions derived from International Satellite Cloud Climatology Project images and latitude time diagrams are used to study the interaction of frontal systems with tropical convection over South America (SA). An 11-yr climatology for three frequent types of frontal system-tropical convection interaction is built, and the associated day-to-day convection variability is described using satellite images, complex principal components, and wavelet transforms. Type 1 is frequent throughout the year, especially in austral summer, and is characterized by the penetration of a cold front in subtropical SA that interacts with tropical convection and moves with it into lower tropical latitudes. Type 2 is also more frequent in austral summer and is characterized by Amazon convection and enhancement of a quasi-stationary northwest-southeast-oriented band of convection extending from the Amazon basin to subtropical SA along the passage of a cold front in the subtropics. When the type 2 pattern remains longer than 4 days over SA, it often characterizes the South Atlantic convergence zone. Type 3, which is more frequent in austral winter, is represented by a quasi-stationary cold front in subtropical SA and midlatitudes without significant interaction with tropical convection. Predominant day-to-day fluctuation time scales of convection associated with the three types were identified, ranging from 5 to 7 days in the Tropics (types 1 and 2) and subtropics (type 3). By evaluating circulation patterns over SA using National Centers for Environmental Prediction analysis at 850 and 200 hPa, the northeastward propagation of a transient cyclonic vortex organized by a cold front in southeast SA and Amazon moisture flows is the main feature of the type 1 pattern at low levels. A cyclonic vortex similar to the one in type 1 but quasi-stationary in the subtropics is remarkable for the type 2 pattern, while upper-level cyclonic vortices in northeast Brazil and the existence of a subtropical jet seem to contribute to the blocking configuration of cold fronts in subtropical SA that characterizes the type 3 pattern.
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URL dos dadoshttp://urlib.net/ibi/x6e6X3pFwXQZ3DUS8rS5/BGDdi
URL dos dados zipadoshttp://urlib.net/zip/x6e6X3pFwXQZ3DUS8rS5/BGDdi
Idiomaen
Arquivo AlvoSiqueira_Influence of the Frontal.pdf
Grupo de Usuáriosadministrator
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentodenypublisher6 allowfinaldraft
Permissão de Leituraallow from all
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 1
DivulgaçãoWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository 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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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriocptec.inpe.br/walmeida/2004/07.23.10.22   (acesso restrito)
Última Atualização2004:12.08.02.00.00 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/walmeida/2004/07.23.10.22.28
Última Atualização dos Metadados2021:02.10.23.11.30 (UTC) administrator
Chave SecundáriaINPE-11148-PRE/6604
ISSN0143-1161
Chave de CitaçãoVilaMach:2004:ShRaPr
TítuloShape and radiative properties of convective systems observed from infrared satellite images
Ano2004
Data de Acesso26 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho421 KiB
2. Contextualização
Autor1 Vila, Daniel A.
2 Machado, Luiz Augusto Toledo
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHMS
Grupo1 DSA-INPE-MCT-BR
2 DSA-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
2 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
Endereço de e-Mailatus@cptec.inpe.br
RevistaInternational Journal of Remote Sensing
Volume25
Páginas1-16
Histórico (UTC)2006-04-04 18:08:31 :: Fabia -> administrator ::
2008-06-10 19:50:42 :: administrator -> estagiario ::
2010-05-11 16:54:05 :: estagiario -> marciana ::
2011-11-01 19:10:58 :: marciana -> administrator ::
2012-11-04 07:15:49 :: administrator -> Fabia :: 2004
2013-02-20 14:49:00 :: Fabia -> administrator :: 2004
2021-02-10 23:11:30 :: administrator -> marciana :: 2004
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 main purpose of this study is to identify a series of parameters to characterize the shape and internal structure of a convective system (CS). One year of brightness temperatures derived from Meteosat 3 (July 1992June 1993) (ISCCP-B3 data) was used to develop this work. The identification of convective systems was performed by pixels whose brightness infrared temperature values (Tir) were below 245 K. The main results obtained are: (a) the shape of a given system can be categorized in three classes: (i) linear systems, (ii) circular and elliptical systems and (iii) fragmented systems; (b) the restitution of a given CS using only statistical information; (c) the identification of the distribution of the number of coldest tops inside a given system; and (d) the evaluation of the stage of the life cycle through a statistical study of internal structure and radiative parameters.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > Shape and radiative...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
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4. Condições de acesso e uso
Idiomaen
Arquivo AlvoVila_Shape and radiative.pdf
Grupo de UsuáriosFabia
administrator
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentodenypublisher denyfinaldraft12
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
DivulgaçãoWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel doi electronicmailaddress format identifier isbn keywords label lineage mark mirrorrepository month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
e-Mail (login)marciana
atualizar