Resultado da Pesquisa
A expressão de busca foi <related:sid.inpe.br/mtc-m21b/2016/05.11.16.18.11-0:en:title:2:level sea rise brazil:integrated framework analyse vulnerability adaptive capacity sea level rise brazil:>.
23 referências similares foram encontradas(inclusive a original) 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: 25/04/2024 09:01.

1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3LLSEGB
Repositóriosid.inpe.br/mtc-m21b/2016/05.11.16.18
Repositório de Metadadossid.inpe.br/mtc-m21b/2016/05.11.16.18.11
Última Atualização dos Metadados2018:06.04.02.40.47 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoMarengoOrsiniNunAlvSouHar:2016:InFrAn
TítuloAn integrated framework to analyse vulnerability and adaptive capacity to sea level rise in Brazil
Ano2016
Data de Acesso25 abr. 2024
Tipo SecundárioPRE CI
2. Contextualização
Autor1 Marengo Orsini, José Antonio
2 Nunes, Luci
3 Alves, Lincoln Muniz
4 Souza, Celia Gouveia
5 Harari, José
Identificador de Curriculo1 8JMKD3MGP5W/3C9JHG3
Grupo1
2
3 CST-CST-INPE-MCTI-GOV-BR
Afiliação1 Centro Nacional de Monitoramento e Alerta de Desastres Naturais (CEMADEN)
2 Universidade Estadual de Campinas (UNICAMP)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Instituto de Geologia
5 Universidade de São Paulo (USP)
Endereço de e-Mail do Autor1
2
3 lincoln.alves@inpe.br
Nome do EventoAdaptation Futures: Practices and Solutions: International Climate Change Adaptation Conference, 4
Localização do EventoRotterdam
Data10-13 May
Histórico (UTC)2016-05-11 16:18:11 :: simone -> administrator ::
2016-07-04 12:30:01 :: administrator -> simone :: 2016
2016-07-08 15:42:13 :: simone -> administrator :: 2016
2018-06-04 02:40:47 :: administrator -> simone :: 2016
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoResearch question: Coastal zones face significant environmental and socio-economic impacts that is already experiencing extreme events. Increased frequency of intense storms events and along with the rise in sea level, lo leads to more coastal flooding. It is extremely important to improve and create tools that allow stakeholders to access reliable science-based information to help them respond to the risks of climate change and sea level raise impacts and assess opportunities for adaptation in coastal areas. Methodology: The location for Brazil is the city of Santos, which is the main port of Brazil. The METROPOLE project is funded by BELMONT Forum. The hypothesis of the project is that risk knowledge is best understood as being co-produced by science and by the social, political and cultural context, engaging stakeholders and policymakers in participatory planning meetings to analyse the social and cultural factors that impact decision-making and regional adaptive capacity. The COastal Adaptation to Sea level rise Tool (COAST) is software that models flooding damage to assets from storm surge and sea level rise over time. It can calculate one-time damages from a single event in time; as well as cumulative damage from all possible storms over a given time period. It then is used to calculate the benefits and costs from various adaptation strategies to determine which strategy is the most fiscal economically efficient over time. A one hundred year storm surge is the height of water with a probability of 0.01. Findings: For Southeast Zone, the damages from storm surge increase greatly from an SLR of 18 cm to 45 cm, and even more for the 1.00 m. with SLR between 18 and 30 cm damages by 2050 are concentrated along the Ponta da Praia neighbourhood. By 2100, Between 30 cm and 1 m the damaged area extends along the coast extending the flooding and storm surges few blocks away from the coast. By 2100, for 1 m SLR, if action is not taken, several areas in Ponta da Praia would be lost due to permanent inundation by SLR. For the Northeast Zone, large areas with high tides due to SLR in the section along the main canal with SLR of 18 to 30 cm, covering a large region and a SLR of 1 m the area flooded can extend until the over most of the region. The estimated damages concentrate mainly along the canal and along the coastal line, with the damages more concentrated (building lost due to flood) mainly in the Sao Manoel region. The cumulative damages shows higher losses for the Southeast zone of Santos, with cumulative losses of $R 1.7 billion with a SLR of 1 m between 2010 and 2100, while the Northwest zone shows losses of $R 550 million. Significance for practical solutions: We show the results of the applications of COAST in Santos, assuming various sea level rise levels until 2100. The partnership with the municipal governments will facilitate the internalization of the results and the implementation of public policies and appropriate environmental legislation and allowing the municipals to better manage their coastal areas.
ÁreaCST
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4. Condições de acesso e uso
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5. Fontes relacionadas
Vinculação8JMKD3MGP3W34P/3L9KTPH
Repositório Espelhourlib.net/www/2011/03.29.20.55
Unidades Imediatamente Superiores8JMKD3MGPCW/3F3T29H
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
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 numberoffiles numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle size sponsor subject targetfile tertiarytype type url versiontype volume
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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/3Q5D2NP
Repositóriosid.inpe.br/mtc-m21b/2017/12.01.15.44
Última Atualização2017:12.01.15.44.29 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2017/12.01.15.44.29
Última Atualização dos Metadados2018:06.04.02.28.03 (UTC) administrator
ISSN2167-9495
2167-9509
Chave de CitaçãoMarengoMPRMNPGLKMGHSAHT:2017:InFrAn
TítuloAn integrated framework to analyze local decision making and adaptation to sea level rise in coastal regions in Selsey (UK), Broward County (USA), and Santos (Brazil)
Ano2017
Data de Acesso25 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho3483 KiB
2. Contextualização
Autor 1 Marengo, J.
 2 Muller-Karger, F.
 3 Pelling, M.
 4 Reynolds, C. J.
 5 Merrill, S. B.
 6 Nunes, L. H.
 7 Paterson, S.
 8 Gray, A. J.
 9 Lockman, J. T.
10 Kartez, J.
11 Moreira, F. A.
12 Greco, R.
13 Harari, J.
14 Souza, C. R. G.
15 Alves, Lincoln Muniz
16 Hosokawa, E. K.
17 Tabuchi, E. K.
Grupo 1
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13
14
15 COCST-COCST-INPE-MCTIC-GOV-BR
Afiliação 1 Centro Nacional de Monitoramento e Alertas de Desastre Naturais (CEMADEN)
 2 University of South Florida
 3 King’s College London
 4 University of South Florida
 5 GEI Consultants Inc
 6 Universidade Estadual de Campinas (UNICAMP)
 7 University College Cork
 8 GEI Consultants Inc
 9 GEI Consultants Inc
10 University of Southern Maine
11 Universidade Estadual de Campinas (UNICAMP)
12 Universidade Estadual de Campinas (UNICAMP)
13 Universidade de São Paulo (USP)
14 Geological Institute of São Paulo
15 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor 1
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13
14
15 lincoln.alves@inpe.br
RevistaAmerican Journal of Climate Change
Volume6
Número2
Páginas403-424
Nota SecundáriaB4_GEOCIÊNCIAS
Histórico (UTC)2017-12-01 15:44:29 :: simone -> administrator ::
2017-12-01 15:44:30 :: administrator -> simone :: 2017
2017-12-01 15:48:42 :: simone -> administrator :: 2017
2017-12-05 18:27:48 :: administrator -> simone :: 2017
2017-12-11 15:53:42 :: simone -> administrator :: 2017
2018-06-04 02:28:03 :: 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
Palavras-ChaveSea Level Rise
Vulnerability
Adaptation
Impacts
Climate Change
ResumoOne of the clear signals of the ongoing climate change is sea level rise (SLR). Normal oceanic tides superimposed on a rising sea level and coastal flooding will affect many coastal communities. An international collaboration among Brazil, the United Kingdom, and the United States was designed to evaluate local decision making processes and to open space for local urban managers to reflect on possible actions toward adaption to sea level rise given the historical constraints imposed by administrative and institutional structures. This project focused on the processes that shape adaptation of three coastal communities in three countries. It worked jointly with these communities in defining the problem, examining risks, and understanding the benefits and obstacles that may hinder implementation of adaptation options. The framework was co-designed by an interdisciplinary team that incorporated social and natural scientists from the three countries, including local government officials. The study addressed 1) evaluation of adaptive capacity through participant surveys and 2) physical and cost impact simulations using geospatial models of the built infrastructure and implementation of adaptation options under different hazard scenarios, including 50 and 100-year sea level rise projections and severe storms. Based on the surveys results, there is a clear sense of the awareness of each community of the risk of floods due to intense storms, and of the usefulness of engaging early in a process that promotes the understanding of risks, impacts, and costs. A majority of workshop participants prioritized pursuing physical and green infrastructure actions now or within coming years or decades. A positive common aspect of the three sites was the commitment shown by the stakeholders in taking part in the process and evaluating which adaptation measures could be more effective in their cities. While in the US and UK structural solutions and voluntary buyouts were prioritized for the future, Brazil prioritized structural solutions and ecosystems restoration and not voluntary buyouts. All of these are choices to increase resiliency against sea level rise that have a high benefit-cost ratio. The Adaptive Capacity Index (ACI) results illustrate barriers to adaptation action, including technical, economic and political issues that reveal inequalities in adaptive capacity among case studies.
ÁreaCST
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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/8JMKD3MGP3W34P/3Q5D2NP
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP3W34P/3Q5D2NP
Idiomaen
Arquivo Alvomarengo.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Vinculação8JMKD3MGP3W34P/3L9KTPH
Repositório Espelhosid.inpe.br/mtc-m21b/2013/09.26.14.25.22
Unidades Imediatamente Superiores8JMKD3MGPCW/3F3T29H
Lista de Itens Citando
DivulgaçãoPORTALCAPES
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel doi e-mailaddress format isbn label lineage mark month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarytype url
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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/3UCTSES
Repositóriosid.inpe.br/mtc-m21c/2019/11.12.09.40   (acesso restrito)
Última Atualização2019:11.12.09.40.25 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21c/2019/11.12.09.40.25
Última Atualização dos Metadados2020:01.06.11.42.23 (UTC) administrator
ISSN2237-8642
Chave de CitaçãoTomazSanBorSilBez:2019:PrImSe
TítuloPredicting the impacts of sea-level rise on the Amazon macrodital mangrove coast
Ano2019
Mêsjul./dez.
Data de Acesso25 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PN
Número de Arquivos1
Tamanho738 KiB
2. Contextualização
Autor1 Tomaz, Raoni
2 Sandos, André
3 Borges, Helder
4 Silva Júnior, Celso Henrique Leite
5 Bezerra, Denilson da Silva
Grupo1
2
3
4 SER-SRE-SESPG-INPE-MCTIC-GOV-BR
Afiliação1 Universidade CEUMA
2 Instituto Federal do Maranhão (IFMA)
3 Instituto Federal do Maranhão (IFMA)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Universidade Federal do Maranhão (UFMA)
Endereço de e-Mail do Autor1 raonibt@gmail.com
2 andresantos@ifma.edu.br
3 helder.borges@ifma.edu.br
4 celso.junior@inpe.br
5 denilson_ca@yahoo.com.br
RevistaRevista Brasileira de Climatologia
Volume25
Páginas15-34
Nota SecundáriaB1_GEOGRAFIA
Histórico (UTC)2019-11-12 09:41:09 :: simone -> administrator :: 2019
2020-01-06 11:42:23 :: administrator -> simone :: 2019
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-ChaveMangrove forests
Amazonian coast
Climate change
Sea-Level Rise
Computational modeling
Geographic Information System
Florestas de manguezal
Costa Amazônica
Mudanças Climáticas
Elevação do Nível do Mar
Modelagem Computacional
Sistema de Informação Geográfica
ResumoBrazil has the largest continuous area of mangrove forests in the world, the Amazon Macrotidal Mangrove Coast (AMMC). The objective of the present study is to simulate the response of eastern Amazonian mangroves to sea-level rise, and to produce a vulnerability assessment for this section of the Brazilian coast. We used a spatially explicit model, based on cellular automata and Geographic Information System (GIS) to identify resistance patterns, migration and/or inundation of these mangroves for different events of sea-level rise (SLR). The simulation considers 90 elevation events from 0.00318 m to 0.2862 m according to an arithmetic progression of reason 0.00318 m for the time interval from 2010 to 2100. The adopted SLR rate was 3.18 mm / year (0.00318 m / year), this rate corresponds to an average of sea elevation values observed for the Brazilian coast during the mid-twentieth century and early twenty-first century. At the end of the simulation (year 2100), the original mangrove area (4,180 km2 ) was reduced to 2,916 km2 , representing a loss of 30.24%. Our simulation also showed significant landward migration of the mangroves, and the modeled loss of the original mangrove area was compensated by a net addition of 301 km2 of new mangroves inland, a net increase of 7.2% in the total mangrove area (4,481 km2 in 2100). These results suggest that mangrove forests in the AMMC can present a pattern of area increase and migration to the continent from the projected SLR. These findings can help the identification of migration corridors for the Amazonian mangroves and the development of adaptation strategies in face of impending SLR. RESUMO: O Brasil possui a maior área contínua de manguezais do mundo, a Costa de Manguezais de Macromarés da Amazônia (CMMA). O objetivo do presente estudo é simular a resposta dos manguezais do leste da Amazônia ao aumento do nível do mar e produzir uma avaliação de vulnerabilidade para este trecho da costa brasileira. Foi utilizado um modelo espacialmente explícito, baseado em autômatos celulares e Sistema de Informações Geográficas (SIG) para identificar padrões de resistência, migração e / ou inundação desses manguezais para diferentes eventos de elevação do nível do mar (ENM). A simulação considera 90 eventos de elevação de 0,00318 m a 0,2862 m de acordo com uma progressão aritmética de razão 0,00318 m para o intervalo de tempo de 2010 a 2100. A taxa ENM adotada foi de 3,18 mm / ano (0,00318 m / ano), esta taxa de elevação corresponde a uma média dos valores de elevação do mar observados para a costa brasileira em meados do século XX e início do século XXI. Ao final da simulação (ano 2100), a área original de manguezal (4.180 km2) foi reduzida para 2.916 km2, representando uma perda de 30,24%. A execução da simulação também mostrou migração significativa do manguezal e a perda modelada da área de manguezal original foi compensada por uma adição líquida de 301 km2 de manguezais para o interior do continente, um aumento líquido de 7,2% na área total de manguezais (4.481 km2 em 2100). Estes resultados sugerem que as florestas de manguezais na CMMA podem apresentar um padrão de aumento de área e migração para o continente a partir da ENM projetada. Essas descobertas podem ajudar na identificação de corredores de migração para os manguezais da Amazônia e no desenvolvimento de estratégias de adaptação frente à ENM iminente.
ÁreaSRE
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Conteúdo da Pasta agreement
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvotomaz_predicting.pdf
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Grupo de Leitoresadministrator
simone
Visibilidadeshown
Permissão de Leituradeny from all and allow from 150.163
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3F3NU5S
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
Campos Vaziosalternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
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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/3P5TAPA
Repositóriosid.inpe.br/plutao/2017/06.21.20.05.41   (acesso restrito)
Última Atualização2017:08.11.18.24.17 (UTC) administrator
Repositório de Metadadossid.inpe.br/plutao/2017/06.21.20.05.42
Última Atualização dos Metadados2021:01.02.03.53.11 (UTC) administrator
DOI10.1007/s11069-017-2855-x
ISSN0921-030X
Rótulolattes: 4336175279058172 14 MarengoNSHMGHTMRPAACMPLG:2017:PuPaCa
Chave de CitaçãoMarengoNSHMGHTMRPAACMPLG:2017:PuPaCa
TítuloA globally deployable strategy for co-development of adaptation preferences to sea-level rise: the public participation case of Santos, Brazil
Ano2017
Data de Acesso25 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho7631 KiB
2. Contextualização
Autor 1 Marengo, José Antonio
 2 Nunes, Luci H.
 3 Souza, Celia R. G.
 4 Harari, Joseph
 5 Muller-Karger, Frank
 6 Greco, Roberto
 7 Hosokawa, Eduardo K.
 8 Tabuchi, Ernesto K.
 9 Merrill, Samuel B.
10 Reynolds, Catherine J.
11 Pelling, Mark
12 Alves, Lincoln Muniz
13 Aragão, Luiz Eduardo Oliveira e Cruz de
14 Chou, Sin Chan
15 Moreira, Fabiano
16 Paterson, Shona
17 Lockman, Jonathan T.
18 Gray, Alexander G.
Grupo 1
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12 COCST-COCST-INPE-MCTIC-GOV-BR
13 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
14 DIDMD-CGCPT-INPE-MCTIC-GOV-BR
Afiliação 1 Centro Nacional de Monitoramento e Alertas de Desastre Naturais (CEMADEN)
 2 Universidade Estadual de Campinas (UNICAMP)
 3 Instituto Geológico
 4 Universidade de São Paulo (USP)
 5 University of South Florida
 6 Universidade Estadual de Campinas (UNICAMP)
 7 Prefeitura de Santos
 8 Prefeitura de Santos
 9 GEI Consultants
10 University of South Florida
11 King’s College London
12 Instituto Nacional de Pesquisas Espaciais (INPE)
13 Instituto Nacional de Pesquisas Espaciais (INPE)
14 Instituto Nacional de Pesquisas Espaciais (INPE)
15 Universidade Estadual de Campinas (UNICAMP)
16 University College Cork
17 GEI Consultants
18 GEI Consultants
Endereço de e-Mail do Autor 1 jose.marengo@cemaden.gov.br
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12 lincoln.alves@inpe.br
13 luiz.aragao@inpe.br
14 chou.chan@inpe.br
RevistaNatural Hazards
Volume8
Número1
Páginas39-53
Nota SecundáriaA1_ENGENHARIAS_I A2_GEOGRAFIA A2_CIÊNCIAS_AGRÁRIAS_I B1_INTERDISCIPLINAR B1_GEOCIÊNCIAS
Histórico (UTC)2017-06-21 20:05:42 :: lattes -> administrator ::
2017-06-23 17:19:08 :: administrator -> lattes :: 2017
2017-06-23 17:24:19 :: lattes -> administrator :: 2017
2017-07-03 05:06:44 :: administrator -> lattes :: 2017
2017-12-05 15:59:03 :: lattes -> administrator :: 2017
2017-12-10 15:16:43 :: administrator -> lattes :: 2017
2017-12-14 10:53:57 :: lattes -> administrator :: 2017
2021-01-02 03:53:11 :: 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
ÁreaCST
Arranjo 1urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > A globally deployable...
Arranjo 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > COCST > A globally deployable...
Arranjo 3urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > A globally deployable...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo Alvomarengo_globally.pdf
Grupo de Leitoresadministrator
lattes
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft12
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
8JMKD3MGPCW/3F3T29H
8JMKD3MGPCW/43SKC35
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.19.20.40 4
sid.inpe.br/bibdigital/2013/09.13.21.11 2
sid.inpe.br/bibdigital/2021/01.01.17.20 1
DivulgaçãoWEBSCI
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosabstract alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn keywords lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url usergroup
7. Controle da descrição
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atualizar 

1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/36P35BB
Repositóriosid.inpe.br/mtc-m19@80/2010/01.11.18.15
Repositório de Metadadossid.inpe.br/mtc-m19@80/2010/01.11.18.15.52
Última Atualização dos Metadados2018:06.05.04.36.09 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoMIRANDARoss:2009:QuPaRe
TítuloQuaternary paleoenvironments and relative sea-level changes in marajó island (northern brazil)
Ano2009
Data de Acesso25 abr. 2024
Tipo SecundárioPRE CN
2. Contextualização
Autor1 MIRANDA, Maria Carolina da Cruz
2 Rossetti, D. F.
Grupo1
2 DSR-OBT-INPE-MCT-BR
Afiliação1
2 undefined
Endereço de e-Mailmarciana@sid.inpe.br
Nome do EventoCongresso Latino Americano de Sedimentologia, 5.
Localização do EventoPuerto La Cruz
Data2009
Histórico (UTC)2010-01-12 11:15:20 :: marciana@sid.inpe.br -> administrator ::
2018-06-05 04:36:09 :: administrator -> marciana@sid.inpe.br ::
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ÁreaSRE
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administrator
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5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosabstract archivingpolicy archivist booktitle callnumber copyholder copyright creatorhistory descriptionlevel dissemination documentstage doi edition editor electronicmailaddress format isbn issn keywords label language lineage mark nextedition notes numberoffiles numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup resumeid rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle size sponsor subject targetfile 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
IdentificadorJ8LNKAN8RW/34BESB4
Repositóriodpi.inpe.br/plutao@80/2008/12.04.12.33.29   (acesso restrito)
Última Atualização2015:04.16.19.32.33 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao@80/2008/12.04.12.33.31
Última Atualização dos Metadados2018:06.05.00.20.02 (UTC) administrator
DOI10.1002/jqs.1132
Rótulolattes: 0307721738107549 1 RossettiValeGóesThal:2008:PaMaIs
Chave de CitaçãoRossettiValeGóesThal:2008:PaMaIs
TítuloPalaeodrainage on Marajó Island,northern Brazil, in relation to Holocene relative sea-level dynamics
Ano2008
Data de Acesso25 abr. 2024
Tipo de Trabalhojournal article
Número de Arquivos1
Tamanho3154 KiB
2. Contextualização
Autor1 Rossetti, Dilce de Fátima
2 Valeriano, Márcio de Morisson
3 Góes, Ana Maria
4 Thallês, Marcelo
Grupo1 DSR-OBT-INPE-MCT-BR
2 DSR-OBT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Universidade de São Paulo (USP)
4 Museu Paraense Emílio Goeldi
Endereço de e-Mail do Autor1 rossetti@dsr.inpe.br
2 valerian@dsr.inpe.br
Endereço de e-Mailrossetti@dsr.inpe.br
RevistaHolocene
Volume18
Número5
Páginas923-934
Histórico (UTC)2008-12-04 16:12:41 :: lattes -> simone ::
2008-12-05 15:19:06 :: simone -> marcia ::
2008-12-15 13:37:49 :: marcia -> administrator ::
2008-12-17 03:45:09 :: administrator -> marciana ::
2013-03-04 16:03:13 :: marciana -> administrator ::
2018-06-05 00:20:02 :: administrator -> marciana :: 2008
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-Chavegeomorfologia
Ilha do Marajó
paleodrenagem
AMBIENTE DEPOSICIONAL
Quaternário
ambientes deposicionais
ResumoA large area in northeastern Marajó Island, northern Brazil, has been characterized geomorphologically, applying information acquired from Landsat imagery. This study was combined with detailed sedimentologic analysis of continuous cores, which provided a record of depositional settings developed in this area through the Holocene. The results revealed well-preserved, meandering to anastomosed drainage networks of wide palaeochannels that were superimposed by a narrower palaeochannel system. In both cases, the sedimentary record consists of sands, heterolithic deposits and muds, locally rich in plant debris. The strata are organized into fining upward successions that reach approximately 18 m thick in the wide channels and 4 m thick in the narrow channels. Sedimentary features suggestive of a coastal location for the wider palaeochannels and reworking of sediments by tidal currents include the prevalence of well to moderately sorted, rounded to subrounded, fine- to medium-grained sands displaying foreset packages separated by mud couplets, suggestive of tidal cycles. The data presented herein point to a rise in relative sea level reaching the Lake Arari area during the early to late/mid Holocene. This event was followed by a relative sea level drop. Tectonics seem to have contributed to an overall lowering in relative sea level in the study area since the mid-Holocene, which does not follow the same pattern recorded in other areas along the northern Brazilian coast.
ÁreaSRE
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Lista de Itens Citandosid.inpe.br/bibdigital/2013/09.13.21.11 1
DivulgaçãoWEBSCI
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
NotasSetores de Atividade: Outros setores.
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn issn lineage mark mirrorrepository month nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate secondarykey secondarymark secondarytype session shorttitle sponsor subject targetfile tertiarymark tertiarytype url
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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/395S5HH
Repositóriosid.inpe.br/mtc-m19/2011/02.08.12.16
Última Atualização2011:02.08.12.16.07 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m19/2011/02.08.12.16.07
Última Atualização dos Metadados2018:06.05.04.35.29 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoRossettiBGVAMTB:2010:LaPlRe
TítuloThe late Pleistocene-Holocene record of sea level in Northeastern Brazil and its relation to climate, eustasy and tectonics
FormatoOn-line
Ano2010
Data de Acesso25 abr. 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho440 KiB
2. Contextualização
Autor1 Rossetti, D
2 Bezerra, F H
3 Góes, A
4 Valeriano, M
5 Andrades Filho, C
6 Millani, J
7 Tatumi, S
8 Brito Neves, B B
Grupo1 DSR-OBT-INPE-MCT-BR
2
3
4 DSR-OBT-INPE-MCT-BR
5 DSR-OBT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2
3 USP, São Paulo, Brazil
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 FATEC, São Paulo, Brazil
7 FATEC, São Paulo, Brazil
8 USP, São Paulo, Brazil
Nome do EventoMeeting of the Americas.
Localização do EventoFoz Iguaçu
Data8-12 Aug. 2010
Título do LivroProceedings
Histórico (UTC)2011-02-08 12:58:01 :: marciana -> administrator :: 2010
2018-06-05 04:35:29 :: administrator -> marciana :: 2010
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Tipo do ConteúdoExternal Contribution
ResumoAB: Late Quaternary deposits in Northeastern Brazil have been scarcely investigated, despite their great relevance to discuss the post-rift evolution of South American passive margin within the context of landform, sea level and tectonic deformation. Sedimentological, stratigraphic and morphological characterization of these deposits led to their distinction from the underlying Early/Middle Miocene Barreiras Formation. Two sedimentary units (PB1 and PB2) were recognized and related, with basis on optically stimulated luminescence (OSL) dating, to the time intervals between 74.8±9.3 and 30.8±6.9 ka, and 8.8±0.9 and 1.8±0.2 ka, respectively. Unit PB1 is exposed discontinuously in the highest topography (usually between 100 m and 150 m), being mostly composed of endured sandstones and breccias either with massive bedding or an abundance of complex styles of ductile and brittle soft sediment deformation structures related to contemporaneous seismic activity. This unit also includes a large volume of non-indured sharply bounded, fining upward massive or stratified conglomerates and sandstones interbedded with mudstones, attributed to fluvial, alluvial and aeolian dune environments. These deposits might include nearshore marine-influenced strata in areas located nearby the modern coastline, as suggested by presence of burrows as Skolithos, Thalassinoides, Planolites, Diplocraterion, and Teichichnus. Unit PB2, composed of sands with massive or dissipation dune structures, occurs continuously, mostly on northeastward dipping tablelands located at altitudes lower than 100 m. The present work focusing on units PB1 and PB2, together referred as Post-Barreiras Sediments, opens a new opportunity to discuss landform, sea level and tectonic history of eastern South American passive margin during the latest Quaternary. Hence, following the Miocene transgression, there was a prolonged period of non-deposition and sub-aerial exposure, which is related to combination of a worldwide low sea level in the Tortonian and tectonic quiescence. Sediment deposition was reactivated during the latest Pleistocene due to tectonic deformation, which created space to accommodate unit PB1 in downthrown faulted blocks and, perhaps, also synclines produced by extension and compression associated with strike-slip tectonic deformation. Although deposition of this unit was simultaneous to the eustatic fall that followed the Penultimate Transgression, punctuated rises superimposed on the overall fall, added to subsidence, would have favored marine deposition in areas located nearby the modern coastline. A renewed phase of deformation would have resulted in newly subsiding areas in the Holocene, promoting deposition of unit PB2 over unit PB1. Although unit PB2 formed during most of the last transgression, except along coastal areas, it has no records of marine sedimentation, suggesting a non-significant rise or reworking of thin transgressive sands by aeolian process. The data presented herein leads to review the evolution of South American passive margin based on assumptions of uniform sedimentation and undeformed planation surfaces over a wide coastal area of Northeastern Brazil.
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Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosarchivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor electronicmailaddress isbn issn keywords label lineage mark nextedition notes numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup 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 Evento (Conference Proceedings)
Sitemtc-m12.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriosid.inpe.br/iris@1912/2005/07.21.01.17
Repositório de Metadadossid.inpe.br/iris@1912/2005/07.21.01.17.09
Última Atualização dos Metadados2018:06.05.00.40.28 (UTC) administrator
Chave SecundáriaINPE-9632-PRE/5248
Rótulo11377
Chave de CitaçãoViannaMene:2002:CuSeLe
TítuloCurrents and sea level off the Northeast Brazilian coast
Ano2002
Data Secundária20021019
Data de Acesso25 abr. 2024
Tipo SecundárioPRE CN
2. Contextualização
Autor1 Vianna, Marcio L.
2 Menezes, Viviane V. de
Grupo1 DSR-INPE-MCT-BR
Nome do EventoSimpósio Brasileiro de Oceanografia, 1.
Localização do EventoSão Paulo
Data26-30 ago. 2002
Histórico (UTC)2008-06-09 22:17:26 :: administrator -> jefferson ::
2010-07-07 19:06:27 :: jefferson -> administrator ::
2018-06-05 00:40:28 :: administrator -> marciana :: 2002
3. Conteúdo e estrutura
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Tipo do ConteúdoExternal Contribution
Palavras-ChaveOCEANOGRAFIA
ResumoThe region of the North Brazil Current (NBC)Retroflection in the northern hemisphere has been studied since the 80ïs by Johns and collaborators (Johns et al., 1998), who disclosed the importance of the annual cycle, the 25-40 day and 60-90 day oscillations in relation to NBC ring shedding. Upstream, with no rings in the NBC, near Fortaleza, no long-term data was ever published to date. This work describes our effort to study sea level and currents over the NE Brazil shelf in the last 8 years. We deployed and maintained 3 Tide Gauges (TG)at Fortaleza and TERMISA over the northern shelf (3S-4S)and at Tamandaré (8S), and two ADCP bottom moorings, and obtained some time series data kindly given to us by INPH and Petrobrás. There are presently three current meter time series records available: two ADCP moorings (July 2000-March 2001, 20m and 30m depths, 037W)at the mid and outer shelf, and one standard current meter mooring off Paracurú (August 1995-March 1996, 40m isobath, 039W, surface data). Hourly wind station data sets from two stations were also made available to us, one at the coast and one at the offshore site off Paracurú. The ADCP data were studied by EOF analysis, which confirmed the well-known barotropic nature of the observed currents on the continental shelf. The principal component time series were analyzed by Multichannel Singular Spectrum Analysis (MSSA). After removal of tidal signals, the low-frequency signal vector spectra show a dominant spectral peak at 57 day period at both ADCP sites, with currents strongly polarized in the longshore direction. The Paracuru currents, and the contemporaneous TG data, present the same spectral bands as the Johns current meter data. These oscillations are shown to be wind-forced by a complex EOF-MSSA analysis. We also used ERS wind scatterometer data to extend this analysis to the NBC Retroflection area, and obtained similar correlation. The annual and interannual variability study was done by use of the TG data, which was shown to be consistent with our altimeter data described in another work in this Symposium. The study shows that while the annual cycle may be absent south of 4S, which is dominated by a biennial cycle, but it is present north of 4S, with a interannual modulation. This is interpreted as a consequence of the fact that the NBC-NBUC south of 4S has a negligible annual cycle, while the C-SEC has a strong one. It is also shown that large phase differences (time scale of a week)between the annual cycle on sites at relative distances of 200 km may be a consequence of interference patterns of incident and scattered equatorially-trapped Rossby waves by the NE coast.
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6. Notas
Campos Vaziosaffiliation archivingpolicy archivist booktitle callnumber copyholder copyright creatorhistory descriptionlevel documentstage doi e-mailaddress edition editor electronicmailaddress format identifier isbn issn lineage mark mirrorrepository nextedition notes numberoffiles numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup readpermission resumeid rightsholder schedulinginformation secondarymark serieseditor session shorttitle size sponsor subject targetfile tertiarymark tertiarytype type url versiontype volume
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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
Identificador8JMKD3MGP5W34M/3FA45DL
Repositóriosid.inpe.br/mtc-m21b/2013/11.26.16.54.36   (acesso restrito)
Última Atualização2014:04.14.17.47.00 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2013/11.26.16.54.37
Última Atualização dos Metadados2018:06.04.03.14.12 (UTC) administrator
DOI10.2458/azu_js_rc.55.16210
ISSN0033-8222
Rótuloscopus 2013-11
Chave de CitaçãoBusoJrPOGCVOTRLBSBFGS:2013:PaEvCo
TítuloFrom an estuary to a freshwater lake: A paleo-estuary evolution in the context of holocene sea-level fluctuations, SE Brazil
ProjetoFAPESP (grants 2007/03615-5, 2007/06222-4, 2010/18091-4, and 2011/00995-7).
Ano2013
Data de Acesso25 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1327 KiB
2. Contextualização
Autor 1 Buso Junior, Antonio Alvaro
 2 Pessenda, Luiz Carlos Ruiz
 3 Oliveira, Paulo Eduardo de
 4 Giannini, Paulo César Fonseca
 5 Cohen, Marcelo Cancela Lisboa
 6 Volkmer-Ribeiro, Cecília
 7 Oliveira, Sonia Maria Barros de
 8 Teixeira Favaro, Deborah Ines
 9 Rossetti, Dilce de Fatima
10 Lorente, Flávio Lima
11 Borotti Filho, Marcos Antonio
12 Schiavo, Jolimar Antonio
13 Bendassolli, José Albertino
14 França, Marlon Carlos
15 Guimarães, José Tasso Felix
16 Siqueira, Geovane Souza
Identificador de Curriculo 1
 2
 3
 4
 5
 6
 7
 8
 9 8JMKD3MGP5W/3C9JGTQ
Grupo 1
 2
 3
 4
 5
 6
 7
 8
 9 DSR-OBT-INPE-MCTI-GOV-BR
Afiliação 1 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
 2 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
 3 São Francisco University, Brazil
 4 Instituto de Geociências da Universidade de São Paulo, Brazil
 5 Federal University of Pará, Brazil
 6 Fundação Zoobotânica do Rio Grande do Sul, Brazil
 7 Instituto de Geociências da Universidade de São Paulo, Brazil
 8 Instituto de Pesquisas Energéticas e Nucleares, Brazil
 9 Instituto Nacional de Pesquisas Espaciais (INPE)
10 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
11 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
12 Universidade Estadual de Mato Grosso do Sul, Brazil
13 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
14 Instituto de Geociências, Univ. Federal do Pará (UFPA), Brazil
15 Instituto de Geociências, Univ. Federal do Pará (UFPA), Brazil
16 Vale Nature Reserve, Brazil
Endereço de e-Mail do Autor 1 alvaro.buso.jr@gmail.com
 2
 3
 4
 5
 6
 7
 8
 9 rossetti@dsr.inpe.br
Endereço de e-Mailmarcelo.pazos@inpe.br
RevistaRadiocarbon
Volume55
Número2-3
Páginas1735-1746
Nota SecundáriaA1 A1 A1 A2 A2 B1 B1
Histórico (UTC)2018-06-04 03:14:12 :: administrator -> :: 2013
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-Chavebasin analysis
coastal zone
estuarine ecosystem
flooding
floodplain
Holocene
ocean basin
sea level change
valley
Brazil
ResumoA sediment core was studied to characterize the influences of Holocene sea-level variations in the Barra Seca River valley, in the Atlantic rainforest, Linhares, Espírito Santo, southeastern Brazil. Biological proxies (pollen, spores, and sponge spicules), 14C dating, granulometry, ´13C, ´15N, C/N and major chemical elements revealed the establishment and the evolution of a paleo-estuary during the interval from ~7700-585 cal BP. During the interval ~7700-7000 cal BP, the study site was occupied by a bay-head delta, the inner portion of the paleo-estuary, presenting the most dense mangrove coverage of the entire record. In the interval ~7000-3200 cal BP, the site was occupied by the central basin, possibly a consequence of the landward migration of the paleo-estuary. This interval presents reduced mangrove coverage, probably due to the permanent flooding of the valley. From ~3200 cal BP, the marine influence at the site decreased probably as result of the seaward migration of the coast line. From ~600 cal BP, the modern floodplain and freshwater lake were established. This interpretation is in agreement with the sea-level curves for the southeastern Brazilian coast, except for the fact that evidence of sea levels lower than the present at ~4000 and ~2500 cal BP as suggested by some authors were not found.
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Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.44.37 1
DivulgaçãoWEBSCI; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
NotasProceedings of the 21st International Radiocarbon Conference
Campos Vaziosalternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark month nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3PJ5EAH
Repositóriosid.inpe.br/mtc-m21b/2017/09.04.19.37   (acesso restrito)
Última Atualização2017:09.04.19.37.14 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2017/09.04.19.37.14
Última Atualização dos Metadados2018:06.04.02.27.49 (UTC) administrator
DOI10.1177/0309133317709744
ISSN0309-1333
Chave de CitaçãoAlvesRoss:2017:LaHoCo
TítuloLate Holocene coastal dynamics and relative sea-level changes in the littoral of Paraiba, northeastern Brazil
Ano2017
MêsAug.
Data de Acesso25 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho3384 KiB
2. Contextualização
Autor1 Alves, Fábio Corrêa
2 Rossetti, Dilce de Fátima
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JGTQ
Grupo1 SER-SRE-SESPG-INPE-MCTIC-GOV-BR
2 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 alves.fabioc@gmail.com
2 dilce.rossetti@inpe.br
RevistaProgress in Physical Geography
Volume41
Número4
Páginas375-392
Nota SecundáriaB1_BIODIVERSIDADE
Histórico (UTC)2017-09-04 19:37:32 :: simone -> administrator :: 2017
2017-10-06 12:36:50 :: administrator -> simone :: 2017
2017-12-11 15:50:36 :: simone -> administrator :: 2017
2018-06-04 02:27:49 :: 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
Palavras-ChavePrograding shoreline
beach ridge
remote sensing
late Holocene
sea-level
ResumoA preliminary analysis of a segment of the Paraiba littoral in northeastern Brazil revealed a prograding shoreline in a coast currently characterized by estuarine transgressive depositional systems. Detailed study of coastal geomorphology is of relevance to reconstruct the sea-level history in this shoreline. Such investigation can help improve the record of past sea-level curves of northeastern Brazil, an issue still open to debates. In this work, we explored remote sensing imagery for the geomorphological characterization of this prograding shoreline and combined this information with geological field data aiming to establish the various phases of shoreline progradation. In addition, we also analyzed the potential forcing factors responsible for the morphological changes in the eastern section of the littoral of Paraiba during the late Holocene, comparing changes with other prograding shorelines along the east coast of Brazil. Geomorphological interpretation was based on the analysis of Phased Array type L-band Synthetic Aperture Radar (PALSAR) images acquired aboard the Advanced Land Observing Satellite 1 (ALOS-1). Geological data comprised dating of sand samples by the optically stimulated luminescence (OSL) technique for the establishment of the chronological context. The coastal deposits are represented by a cuspate morphology and numerous internal beach ridges that prograded seaward from a roughly north-south trending palaeocliff. The chronological data indicate shoreline progradation during the past 2.1 +/- 0.1 ka, after the mid-Holocene sea-level fall. Several prograding episodes occurred during this time, some not matching with proposed sea-level rises punctuated upon the overall fall. Together with the regional geological context of the study area, we propose that eustatic sea-level was not the only factor triggering coastal progradation in this region.
ÁreaSRE
Arranjo 1urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Late Holocene coastal...
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvoalves_late.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Vinculação8JMKD3MGP7W/3J3BGME
Repositório Espelhosid.inpe.br/mtc-m21b/2013/09.26.14.25.22
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
8JMKD3MGPCW/3F3NU5S
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.18.22.34 1
sid.inpe.br/mtc-m21/2012/07.13.14.44.37 1
DivulgaçãoWEBSCI; PORTALCAPES; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarytype url
7. Controle da descrição
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