1. Identificação | |
Tipo de Referência | Artigo em Revista Científica (Journal Article) |
Site | plutao.sid.inpe.br |
Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identificador | J8LNKAN8RW/35LDKUM |
Repositório | dpi.inpe.br/plutao@80/2009/07.13.15.12.55 (acesso restrito) |
Última Atualização | 2010:09.20.13.43.20 (UTC) administrator |
Repositório de Metadados | dpi.inpe.br/plutao@80/2009/07.13.15.12.56 |
Última Atualização dos Metadados | 2018:06.05.00.12.40 (UTC) administrator |
Chave Secundária | INPE--PRE/ |
ISSN | 0703-8992 |
Rótulo | lattes: 6262085938550551 8 SilvaKRSROR:2009:EfMiRA |
Chave de Citação | ParadellaSKRSROR:2009:EfMiRA |
Título | Effect of Microtopography on RADARSAT-1 and PALSAR Backscattering from Rock Alteration Products in the Curaçá Valley, Brazil |
Ano | 2009 |
Mês | June |
Data de Acesso | 12 maio 2024 |
Tipo de Trabalho | journal article |
Tipo Secundário | PRE PI |
Número de Arquivos | 1 |
Tamanho | 5743 KiB |
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2. Contextualização | |
Autor | 1 Paradella, Waldir Renato 2 Silva, Arnaldo Queiroz da 3 Knust, S. S. A 4 Rabelo, T. N. 5 Santos, Athos Ribeiro 6 Rennó, Camilo Daleles 7 Oliveira, Cleber Ganzolive 8 Rodrigues, Thiago Gonçalves |
Grupo | 1 DSR-OBT-INPE-MCT-BR 2 DSR-OBT-INPE-MCT-BR 3 DSR-OBT-INPE-MCT-BR 4 DSR-OBT-INPE-MCT-BR 5 DSR-OBT-INPE-MCT-BR 6 DPI-OBT-INPE-MCT-BR 7 DSR-OBT-INPE-MCT-BR 8 DSR-OBT-INPE-MCT-BR |
Afiliação | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Instituto Nacional de Pesquisas Espaciais (INPE) 4 Instituto Nacional de Pesquisas Espaciais (INPE) 5 Instituto Nacional de Pesquisas Espaciais (INPE) 6 Instituto Nacional de Pesquisas Espaciais (INPE) 7 Instituto Nacional de Pesquisas Espaciais (INPE) 8 Instituto Nacional de Pesquisas Espaciais (INPE) |
Endereço de e-Mail do Autor | 1 2 3 4 5 6 7 8 thiagogr@dsr.inpe.br |
Endereço de e-Mail | thiagogr@dsr.inpe.br |
Revista | Canadian Journal of Remote Sensing |
Volume | 35 |
Número | 3 |
Páginas | 262-269 |
Nota Secundária | B1_CIÊNCIAS_BIOLÓGICAS_I B1_ENGENHARIAS_I B1_GEOCIÊNCIAS |
Histórico (UTC) | 2009-07-13 17:05:13 :: lattes -> marciana :: 2010-04-29 12:32:21 :: marciana -> administrator :: 2010-05-12 02:04:36 :: administrator -> marciana :: 2011-12-07 10:54:20 :: marciana -> administrator :: 2009 2016-06-04 01:08:34 :: administrator -> marciana :: 2009 2016-10-04 17:22:07 :: marciana -> administrator :: 2009 2018-06-05 00:12:40 :: administrator -> marciana :: 2009 |
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3. Conteúdo e estrutura | |
É a matriz ou uma cópia? | é a matriz |
Estágio do Conteúdo | concluido |
Transferível | 1 |
Tipo do Conteúdo | External Contribution |
Tipo de Versão | publisher |
Palavras-Chave | Archean Backscattering coefficients Caatinga Correlation lengths Cross polarizations Geological surface Incidence angles L-band synthetic aperture radars Linear correlation Micro topography Northeastern Brazil Phased arrays Proterozoic RADARSAT 1 Regression coefficient Residual soil Rock alterations Root Mean Square SAR data Semi-arid environments Vegetation cover Backscattering Imaging systems Instrument scales Landforms Radar Regression analysis Rock products Synthetic apertures Synthetic aperture radar |
Resumo | This paper addresses the influence of microtopography (root mean square height HRMS and correlation length LC) on RADARSAT-1 and phased array L-band synthetic aperture radar (PALSAR) backscattering coefficient (σ0) values from distinct rock alteration products of the Cu-rich district of Curaçá Valley, northeastern Brazil. The area is characterized by a semiarid environment, flat topography with rock outcrops and residual soils, and low to moderate Caatinga vegetation cover. The lithologies consist of Archean gneisses and granulites interbedded with mafic-ultramafic intrusives and upper Proterozoic marbles, schists, and phyllites. The images were acquired under distinct look azimuth and incidence angles and corresponded to four RADARSAT-1 images (F2, S2, and S7 ascending and S7 descending) and one PALSAR image (fine beam dual (FBD) descending). The research was based on the use of linear regression analyses, which showed a weak to moderate linear correlation between σ0 and HRMS and LC for both SAR data. HRMS was the most important microtopographic parameter influencing σ0, whereas LC played a secondary role. Regarding RADARSAT-1, the highest regression coefficient (R2) values were obtained for shallower incidence angles (S7), and this dependence increased from steeper to shallower incidence, regardless of changes in the look azimuth. For PALSAR, R2 was slightly higher than that for RADARSAT-1 and was related to cross-polarization. The investigation showed that backscattering for synthetic aperture radar (SAR) data from both RADARSAT-1 and PALSAR is not modulated in a predominant manner by the microtopographic variations of the geological surfaces. |
Área | SRE |
Arranjo 1 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDPI > Effect of Microtopography... |
Arranjo 2 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Effect of Microtopography... |
Conteúdo da Pasta doc | acessar |
Conteúdo da Pasta source | não têm arquivos |
Conteúdo da Pasta agreement | não têm arquivos |
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4. Condições de acesso e uso | |
Idioma | en |
Arquivo Alvo | paradella2.pdf |
Grupo de Usuários | administrator lattes administrator marciana |
Grupo de Leitores | administrator marciana |
Visibilidade | shown |
Permissão de Leitura | deny from all and allow from 150.163 |
Permissão de Atualização | não transferida |
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5. Fontes relacionadas | |
Unidades Imediatamente Superiores | 8JMKD3MGPCW/3EQCCU5 8JMKD3MGPCW/3ER446E |
Divulgação | WEBSCI |
Acervo Hospedeiro | dpi.inpe.br/plutao@80/2008/08.19.15.01 |
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6. Notas | |
Campos Vazios | alternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel doi format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype url |
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7. Controle da descrição | |
e-Mail (login) | marciana |
atualizar | |
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