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4 referências similares encontradas (inclusive a original) buscando em 22 dentre 22 Arquivos.
Data e hora local de busca: 16/05/2024 16:41.
1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/3UHGDM2
Repositóriosid.inpe.br/mtc-m21c/2019/12.10.13.03
Última Atualização2020:11.23.13.13.12 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21c/2019/12.10.13.03.26
Última Atualização dos Metadados2021:01.03.02.12.36 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoSalioCenNesVidVil:2019:EnCoAs
TítuloEnvironmental conditions associated to convective initiation of extreme convective systems over Southeastern South America
Ano2019
Data de Acesso16 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho72 KiB
2. Contextualização
Autor1 Salio, Paola Veronica
2 Cencelada, Maite
3 Nesbitt, Stephen W.
4 Vidal, Luciano
5 Vila, Daniel Alejandro
Grupo1
2
3
4
5 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
Afiliação1 Centro de Investigaciones del Mar y la Atmosfera
2 Centro de Investigaciones del Mar y la Atmosfera
3 University of Illinois at Urbana Champaign
4 Servicio Meteorologico Nacional
5 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1
2
3
4
5 daniel.vila@inpe.br
Nome do EventoAGU Fall Meeting
Localização do EventoSan Francisco, CA
Data09-13 dec.
Histórico (UTC)2020-11-23 13:13:13 :: simone -> administrator :: 2019
2021-01-03 02:12:36 :: administrator -> simone :: 2019
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoMany thunderstorms in Southeastern South America (SESA) stand out in satellite observations as being among the strong on Earth in terms of satellite-based convective proxies, such as lightning flash rate per storm, the prevalence for extremely tall, wide convective cores and broad stratiform regions. Knowing when and where strong convection is initiated presenting a great interest because of the close relationship between convective storms and severe weather phenomena. This paper generates a novel methodology to determine convective initiation areas associated with extreme convective systems. Due to the lack of long records of ground-based radars in the area, Rain Precipitation Features (RPFs) from Global Precipitation Measurement and Tropical Rainfall Measurement Mission are considered to determine extreme convective events, as well as overshooting tops from GOES16 over RELAMPAGO-CACTI field campaign. These different extreme convective events generate a large sample allowing to determine convective initiation areas over SESA during multiple years. All events are tracked backward using an adaptive threshold area-overlapping technique with thermal infrared (IR) channel. It was necessary to consider multiple IR temperature thresholds in order to identify areas of deep convection embedded within larger cloud clusters. Convective initiation diurnal cycle is analyzed near principal mountain barriers (Sierras de Córdoba, central and Northwestern Argentinean Andes), denoting a strong relationship during the afternoon and early evening hours with convergence at mountain ridges. It is also possible to detect convective initiation areas over flat terrain, revealing with a strong initiation signal on nocturnal times. Key features associated with mesoscale and synoptic scale pre-environmental conditions are analyzed over different samples considering initiation times and mountain versus the surrounding plains regions.
ÁreaMET
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP3W34R/3UHGDM2
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP3W34R/3UHGDM2
Idiomaen
Arquivo Alvosalio_environmental.pdf
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5. Fontes relacionadas
Repositório Espelhourlib.net/www/2017/11.22.19.04.03
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 1
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
Campos Vaziosarchivingpolicy archivist booktitle callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor format isbn issn keywords label lineage mark nextedition notes numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readpermission resumeid rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark tertiarytype type url versiontype volume
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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
Identificador8JMKD3MGP3W/3P5TDTE
Repositóriosid.inpe.br/plutao/2017/06.21.20.44
Última Atualização2017:06.23.12.40.13 (UTC) administrator
Repositório de Metadadossid.inpe.br/plutao/2017/06.21.20.44.38
Última Atualização dos Metadados2021:01.03.02.11.11 (UTC) administrator
DOI10.5194/acp-2016-1155
ISSN1680-7367
Rótulolattes: 5379515759830546 14 BragaRWJAWPVMBAMVMG:2017:AeCoDe
Chave de CitaçãoBragaRWJAWPVMBAMVMG:2017:AeCoDe
TítuloAerosol concentrations determine the height of warm rain and ice initiation in convective clouds over the Amazon basin
Ano2017
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho3883 KiB
2. Contextualização
Autor 1 Braga, Ramon Campos
 2 Rosenfeld, Daniel
 3 Weigel, Ralf
 4 Jurkat, Tina
 5 Andreae, Meinrat O.
 6 Wendisch, Manfred
 7 Pöschl, Ulrich
 8 Voigt, Christiane
 9 Mahnke, Christoph
10 Borrmann, Stephan
11 Albrecht, Rachel I.
12 Molleker, Sergej
13 Vila, Daniel Alejandro
14 Machado, Luiz Augusto Toledo
15 Grulich, Lucas
Identificador de Curriculo 1
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13
14 8JMKD3MGP5W/3C9JHMS
Grupo 1 MET-MET-SESPG-INPE-MCTIC-GOV-BR
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
14 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
Afiliação 1 Instituto Nacional de Pesquisas Espaciais (INPE)
 2 The Hebrew University of Jerusalem
 3 Johannes Gutenberg-Universität
 4 Institut für Physik der Atmosphäre
 5 Max Planck Institute for Chemistry
 6 Universität Leipzig
 7 Max Planck Institute for Chemistry
 8 Johannes Gutenberg-Universität
 9 Johannes Gutenberg-Universität
10 Johannes Gutenberg-Universität
11 Universidade de São Paulo (USP)
12 Max Planck Institute for Chemistry
13 Instituto Nacional de Pesquisas Espaciais (INPE)
14 Instituto Nacional de Pesquisas Espaciais (INPE)
15 Johannes Gutenberg-Universität
Endereço de e-Mail do Autor 1 ramonbraga87@gmail.com
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13 daniel.vila@inpe.br
14 luiz.machado@inpe.br
RevistaAtmospheric Chemistry and Physics Discussion
Volume2017
Páginas1-44
Nota SecundáriaC_ASTRONOMIA_/_FÍSICA
Histórico (UTC)2017-06-22 07:58:52 :: lattes -> administrator :: 2017
2017-06-22 08:07:24 :: administrator -> lattes :: 2017
2017-06-29 16:51:54 :: lattes -> administrator :: 2017
2021-01-03 02:11:11 :: administrator -> simone :: 2017
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoWe have investigated how pollution aerosols affect the height above cloud base of rain and ice hydrometeor initiation and the subsequent vertical evolution of cloud droplet size and number concentrations in growing convective cumulus. For this purpose we used in-situ data of hydrometeor size distributions measured with instruments mounted on HALO (High Altitude and Long Range Research Aircraft) during the ACRIDICON-CHUVA campaign over the Amazon during September 2014. The results show that the height of rain initiation by collision and coalescence processes (Dr, in units of meters above cloud base) is linearly correlated with the number concentration of droplets (Nd in cm-3) nucleated at cloud base (Dr ≈ 5·Nd). When Nd exceeded values of about 1000 cm-3, Dr became greater than 5000 m, and particles of precipitation size were initiated as ice hydrometeors. Therefore, no liquid water raindrops were observed within growing convective cumulus during polluted conditions. Furthermore, also the formation of ice particles took place at higher altitudes in the clouds in polluted conditions, because the resulting smaller cloud droplets froze at colder temperatures compared to the larger drops in the unpolluted cases. The measured vertical profiles of droplet effective radius (re) were close to those estimated by assuming adiabatic conditions (rea), supporting the hypothesis that the entrainment and mixing of air into convective clouds is almost completely inhomogeneous. Secondary nucleation of droplets on aerosol particles from biomass burning and air pollution reduced re below rea, which further inhibited the formation of raindrops and ice particles and resulted in even higher altitudes for rain and ice initiation.
ÁreaMET
Arranjo 1urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > Aerosol concentrations determine...
Arranjo 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > Aerosol concentrations determine...
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Conteúdo da Pasta sourcenão têm arquivos
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP3W/3P5TDTE
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP3W/3P5TDTE
Idiomaen
Arquivo Alvobraga_aerosol.pdf
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lattes
Visibilidadeshown
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Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3F35TRS
8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 1
DivulgaçãoWEBSCI; PORTALCAPES; MGA.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn keywords lineage mark mirrorrepository month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project readpermission rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url usergroup
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/425Q9C2
Repositóriosid.inpe.br/mtc-m21c/2020/03.13.14.15
Última Atualização2020:03.13.14.15.50 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21c/2020/03.13.14.15.50
Última Atualização dos Metadados2022:01.04.01.35.01 (UTC) administrator
DOI10.3390/rs12020337
ISSN2072-4292
Chave de CitaçãoCanceladaSalVilNesVid:2020:MeDeEx
TítuloBackward Adaptive Brightness Temperature Threshold Technique (BAB3T): a methodology to determine extreme convective initiation regions using satellite infrared imagery
Ano2020
Mêsjan.
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho10447 KiB
2. Contextualização
Autor1 Cancelada, Maite
2 Salio, Paola
3 Vila, Daniel Alejandro
4 Nesbitt, Stephen W.
5 Vidal, Luciano
ORCID1
2
3 0000-0002-1015-5650
4 0000-0003-0348-0452
Grupo1
2
3 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
Afiliação1 Universidad de Buenos Aires
2 Universidad de Buenos Aires
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 University of Illinois at Urbana-Champaign
5 Servicio Meteorológico Nacional, Buenos Aires
Endereço de e-Mail do Autor1 maite.cancelada@cima.fcen.uba.ar
2 salio@cima.fcen.uba.ar
3 daniel.vila@inpe.br
4 snesbitt@illinois.edu
5 lvidal@smn.gov.ar
RevistaRemote Sensing
Volume12
Número2
Páginase337
Nota SecundáriaB3_GEOGRAFIA B3_ENGENHARIAS_I B4_GEOCIÊNCIAS B4_CIÊNCIAS_AMBIENTAIS B5_CIÊNCIAS_AGRÁRIAS_I
Histórico (UTC)2020-03-13 14:15:50 :: simone -> administrator ::
2020-03-13 14:15:50 :: administrator -> simone :: 2020
2020-03-13 14:16:43 :: simone -> administrator :: 2020
2022-01-04 01:35:01 :: administrator -> simone :: 2020
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-Chaveconvective initiation
satellite observations
algorithms
severe weather
ResumoThunderstorms in southeastern South America (SESA) stand out in satellite observations as being among the strongest on Earth in terms of satellite-based convective proxies, such as lightning flash rate per storm, the prevalence for extremely tall, wide convective cores and broad stratiform regions. Accurately quantifying when and where strong convection is initiated presents great interest in operational forecasting and convective system process studies due to the relationship between convective storms and severe weather phenomena. This paper generates a novel methodology to determine convective initiation (CI) signatures associated with extreme convective systems, including extreme events. Based on the well-established area-overlapping technique, an adaptive brightness temperature threshold for identification and backward tracking with infrared data is introduced in order to better identify areas of deep convection associated with and embedded within larger cloud clusters. This is particularly important over SESA because ground-based weather radar observations are currently limited to particular areas. Extreme rain precipitation features (ERPFs) from Tropical Rainfall Measurement Mission are examined to quantify the full satellite-observed life cycle of extreme convective events, although this technique allows examination of other intense convection proxies such as the identification of overshooting tops. CI annual and diurnal cycles are analyzed and distinctive behaviors are observed for different regions over SESA. It is found that near principal mountain barriers, a bimodal diurnal CI distribution is observed denoting the existence of multiple CI triggers, while convective initiation over flat terrain has a maximum frequency in the afternoon.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > Backward Adaptive Brightness...
Conteúdo da Pasta docacessar
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Conteúdo da Pasta agreement
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP3W34R/425Q9C2
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP3W34R/425Q9C2
Idiomaen
Arquivo Alvoremotesensing-12-00337.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 5
DivulgaçãoWEBSCI; PORTALCAPES; MGA; COMPENDEX; SCOPUS.
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey 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)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3Q8K3S5
Repositóriosid.inpe.br/mtc-m21b/2017/12.21.11.38
Última Atualização2017:12.21.11.38.40 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2017/12.21.11.38.40
Última Atualização dos Metadados2021:01.03.02.11.55 (UTC) administrator
DOI10.5194/acp-17-14433-2017
ISSN1680-7316
1680-7324
Chave de CitaçãoBragaRWJAWPVMBAMVMG:2017:FuEvCC
TítuloFurther evidence for CCN aerosol concentrations determining the height of warm rain and ice initiation in convective clouds over the Amazon basin
Ano2017
MêsDec.
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho6729 KiB
2. Contextualização
Autor 1 Braga, Ramon Campos
 2 Rosenfeld, Daniel
 3 Weigel, Ralf
 4 Jurkat, Tina
 5 Andreae, Meinrat O.
 6 Wendisch, Manfred
 7 Pöschl, Ulrich
 8 Voigt, Christiane
 9 Mahnke, Christoph
10 Borrmann, Stephan
11 Albrecht, Rachel I.
12 Molleker, Sergej
13 Vila, Daniel Alejandro
14 Machado, Luiz Augusto Toledo
15 Grulich, Lucas
Identificador de Curriculo 1
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13
14 8JMKD3MGP5W/3C9JHMS
Grupo 1 MET-MET-SESPG-INPE-MCTIC-GOV-BR
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
14 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
Afiliação 1 Instituto Nacional de Pesquisas Espaciais (INPE)
 2 The Hebrew University of Jerusalem
 3 Johannes Gutenberg-Universität
 4 Deutsches Zentrum für Luft- und Raumfahrt (DLR)
 5 Max Planck Institute for Chemistry
 6 Universität Leipzig
 7 Max Planck Institute for Chemistry
 8 Johannes Gutenberg-Universität
 9 Johannes Gutenberg-Universität
10 Johannes Gutenberg-Universität
11 Universidade de São Paulo (USP)
12 Max Planck Institute for Chemistry
13 Instituto Nacional de Pesquisas Espaciais (INPE)
14 Instituto Nacional de Pesquisas Espaciais (INPE)
15 Johannes Gutenberg-Universität
Endereço de e-Mail do Autor 1 ramonbraga87@gmail.com
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13 daniel.vila@inpe.br
14 luiz.machado@inpe.br
RevistaAtmospheric Chemistry and Physics
Volume17
Páginas14433-14456
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)2017-12-21 11:38:40 :: simone -> administrator ::
2017-12-21 11:38:41 :: administrator -> simone :: 2017
2017-12-21 11:43:02 :: simone -> administrator :: 2017
2021-01-03 02:11:55 :: administrator -> simone :: 2017
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoWe have investigated how aerosols affect the height above cloud base of rain and ice hydrometeor initiation and the subsequent vertical evolution of cloud droplet size and number concentrations in growing convective cumulus. For this purpose we used in situ data of hydrometeor size distributions measured with instruments mounted on HALO aircraft during the ACRIDICONCHUVA campaign over the Amazon during September 2014. The results show that the height of rain initiation by collision and coalescence processes (Dr , in units of meters above cloud base) is linearly correlated with the number concentration of droplets (Nd in cm−3 ) nucleated at cloud base (Dr ≈ 5 · Nd). Additional cloud processes associated with Dr , such as GCCN, cloud, and mixing with ambient air and other processes, produce deviations of ∼ 21 % in the linear relationship, but it does not mask the clear relationship between Dr and Nd, which was also found at different regions around the globe (e.g., Israel and India). When Nd exceeded values of about 1000 cm−3 , Dr became greater than 5000 m, and the first observed precipitation particles were ice hydrometeors. Therefore, no liquid water raindrops were observed within growing convective cumulus during polluted conditions. Furthermore, the formation of ice particles also took place at higher altitudes in the clouds in polluted conditions because the resulting smaller cloud droplets froze at colder temperatures compared to the larger drops in the unpolluted cases. The measured vertical profiles of droplet effective radius (re) were close to those estimated by assuming adiabatic conditions (rea), supporting the hypothesis that the entrainment and mixing of air into convective clouds is nearly inhomogeneous. Additional CCN activation on aerosol particles from biomass burning and air pollution reduced re below rea, which further inhibited the formation of raindrops and ice particles and resulted in even higher altitudes for rain and ice initiation.
ÁreaMET
Arranjo 1urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > Further evidence for...
Arranjo 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > Further evidence for...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
agreement.html 21/12/2017 09:38 1.0 KiB 
4. Condições de acesso e uso
URL dos dadoshttp://mtc-m21b.sid.inpe.br/ibi/8JMKD3MGP3W34P/3Q8K3S5
URL dos dados zipadoshttp://mtc-m21b.sid.inpe.br/zip/8JMKD3MGP3W34P/3Q8K3S5
Idiomaen
Arquivo Alvobraga_further.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
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Visibilidadeshown
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m21b/2013/09.26.14.25.22
Unidades Imediatamente Superiores8JMKD3MGPCW/3F35TRS
8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 3
DivulgaçãoWEBSCI; PORTALCAPES; AGU; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn keywords label lineage mark nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project readpermission rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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