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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/35LDKUM
Repositóriodpi.inpe.br/plutao@80/2009/07.13.15.12.55   (acesso restrito)
Última Atualização2010:09.20.13.43.20 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao@80/2009/07.13.15.12.56
Última Atualização dos Metadados2018:06.05.00.12.40 (UTC) administrator
Chave SecundáriaINPE--PRE/
ISSN0703-8992
Rótulolattes: 6262085938550551 8 SilvaKRSROR:2009:EfMiRA
Chave de CitaçãoParadellaSKRSROR:2009:EfMiRA
TítuloEffect of Microtopography on RADARSAT-1 and PALSAR Backscattering from Rock Alteration Products in the Curaçá Valley, Brazil
Ano2009
MêsJune
Data de Acesso12 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho5743 KiB
2. Contextualização
Autor1 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
Grupo1 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
Afiliação1 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 Autor1
2
3
4
5
6
7
8 thiagogr@dsr.inpe.br
Endereço de e-Mailthiagogr@dsr.inpe.br
RevistaCanadian Journal of Remote Sensing
Volume35
Número3
Páginas262-269
Nota SecundáriaB1_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
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-ChaveArchean
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
ResumoThis 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.
ÁreaSRE
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Conteúdo da Pasta sourcenão têm arquivos
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvoparadella2.pdf
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EQCCU5
8JMKD3MGPCW/3ER446E
DivulgaçãoWEBSCI
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal 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
7. Controle da descrição
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