Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment

Detalhes bibliográficos
Autor(a) principal: Carlos Alexandre Gomes Costa
Data de Publicação: 2008
Tipo de documento: Dissertação
Idioma: por
Título da fonte: Biblioteca Digital de Teses e Dissertações da UFC
Texto Completo: http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=5229
Resumo: Face to global climate change it is necessary a better understanding of the hydrological and environmental dynamics. To characterize them in a short time with reliability is an important requirement for the science. Topography is a major factor to understand these factors. Its determination is onerous, both economically and temporally, and the dynamics of environmental transformations that alters its pattern must be considered. In the year 2000, through a interferometric RADAR topographic mission (SRTM) led by NASA in cooperation with the German (DRL) and the Italian (ASI) space agencies, a Digital Elevation Model was generated by the employment of RADAR interferometry. These data are available costless and have been greatly used by scientists. Nonetheless, since it is a RADAR interferometer product, it represents the Earth surface and is subjected to the influence of vegetation, what may make this DEM unriliable in works that require a high detail level and good precision. Therefore, the objective of this research is to validate SRTM data to the Brazilian semi-arid conditions and, based on these data, characterize the physiograph of watersheds in the Jaguaribe basin. The methodology used in the SRTM data validation consists in a comparison and statistical analysis of field data obtained with a differential GPS (DGPS) and other data bases such as the DSG/SUDENE maps and level reference points from IBGE in the Jaguaribe basin located in Cearà State. Results present an elevation error of approximately 7 m in relation to the level reference points in the basin. For the use of DGPS on a plan relief with very low slopes and vegetation with low heights, results show an elevation error of approximately 1.7 m. Vegetation cover influenced the variation in SRTM data to vegetation with higher mean height. To the physiographic characterization, values not larger than 50 pixels must be adopted as the contributing area of SRTM (90m), used in the generation of the river network and the Hydrological Consistent Digital Elevation Model (HCDEM) in the study area. To areas with low slopes, the threshold value must be reviewed. The development of a reference bibliography with physiographic characterization associated to the use of a Geographic Information System (GIS) and a DEM is fundamental as it enhances the possibilities of generating products from remote sensing and geo-processing techniques. The use of ArcHydro extension facilitates a physiographic characterization and allows the storage and use of these data as a GIS.
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spelling info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisAssessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environmentAvaliaÃÃo dos dados SRTM atravÃs de anÃlise altimÃtrica e morfomÃtrica de bacias hidrogrÃficas no Semi-Ãrido.2008-03-28Adunias dos Santos Teixeira33344423453http://lattes.cnpq.br/9646492923898649Eunice Maia de Andrade11748729349http://lattes.cnpq.br/7012348447122522Marco AurÃlio Holanda de Castro2795889218775153033368http://lattes.cnpq.br/9346087418658759Carlos Alexandre Gomes CostaUniversidade Federal do CearÃPrograma de PÃs-GraduaÃÃo em Engenharia AgrÃcolaUFCBRIRRIGACAO E DRENAGEMFace to global climate change it is necessary a better understanding of the hydrological and environmental dynamics. To characterize them in a short time with reliability is an important requirement for the science. Topography is a major factor to understand these factors. Its determination is onerous, both economically and temporally, and the dynamics of environmental transformations that alters its pattern must be considered. In the year 2000, through a interferometric RADAR topographic mission (SRTM) led by NASA in cooperation with the German (DRL) and the Italian (ASI) space agencies, a Digital Elevation Model was generated by the employment of RADAR interferometry. These data are available costless and have been greatly used by scientists. Nonetheless, since it is a RADAR interferometer product, it represents the Earth surface and is subjected to the influence of vegetation, what may make this DEM unriliable in works that require a high detail level and good precision. Therefore, the objective of this research is to validate SRTM data to the Brazilian semi-arid conditions and, based on these data, characterize the physiograph of watersheds in the Jaguaribe basin. The methodology used in the SRTM data validation consists in a comparison and statistical analysis of field data obtained with a differential GPS (DGPS) and other data bases such as the DSG/SUDENE maps and level reference points from IBGE in the Jaguaribe basin located in Cearà State. Results present an elevation error of approximately 7 m in relation to the level reference points in the basin. For the use of DGPS on a plan relief with very low slopes and vegetation with low heights, results show an elevation error of approximately 1.7 m. Vegetation cover influenced the variation in SRTM data to vegetation with higher mean height. To the physiographic characterization, values not larger than 50 pixels must be adopted as the contributing area of SRTM (90m), used in the generation of the river network and the Hydrological Consistent Digital Elevation Model (HCDEM) in the study area. To areas with low slopes, the threshold value must be reviewed. The development of a reference bibliography with physiographic characterization associated to the use of a Geographic Information System (GIS) and a DEM is fundamental as it enhances the possibilities of generating products from remote sensing and geo-processing techniques. The use of ArcHydro extension facilitates a physiographic characterization and allows the storage and use of these data as a GIS.Em tempos de mudanÃas globais torna-se necessÃrio cada vez mais entender a dinÃmica hidrolÃgica e ambiental. CaracterizÃ-las em um menor tempo possÃvel, com maior confiabilidade à a exigÃncia imperativa que pesa sobre a ciÃncia. A topografia evidencia-se como um fator imprescindÃvel no entendimento destes processos. Sua determinaÃÃo à onerosa, tanto economicamente quanto temporalmente, tendo ainda que considerar a dinÃmica das transformaÃÃes ambientais que alteram continuamente essa topografia.. Em 2000 atravÃs da missÃo topogrÃfica por RADAR interferomÃtrico (SRTM), liderada pela NASA com a colaboraÃÃo das agÃncias espaciais alemà (DRL) e italiana (ASI) foi gerado um Modelo Digital de ElevaÃÃo (MDE) utilizando a interferometria de RADAR. Esses dados sÃo disponÃveis gratuitamente e estÃo sendo usados em grande escala no meio cientÃfico. Entretanto, por ser um produto interferometria de RADAR, retrata a superfÃcie da terra, sofrendo inclusive a influÃncia da vegetaÃÃo, o que pode inviabilizar o uso desse MDE em trabalhos que exijam maior nÃvel de detalhamento e precisÃo.. Assim, o objetivo deste trabalho foi validar os dados SRTM para as condiÃÃes do semi-Ãrido brasileiro e a partir destes dados estimar com maior consistÃncia a caracterizaÃÃo fisiogrÃfica de bacias hidrogrÃficas afluentes do rio Jaguaribe. A metodologia utilizada na validaÃÃo dos dados SRTM consiste em comparaÃÃes e anÃlise estatÃstica com dados obtidos no campo com GPS diferencial (DGPS) e outras bases de dados referenciais existentes, cartas planialtimÃtricas DSG/ SUDENE e dados de RN do IBGE para a Bacia do Jaguaribe situada no semi-Ãrido cearense. Os resultados apresentam um erro altimÃtrico de aproximadamente 7 m com relaÃÃo aos RNs da bacia. Com uso do DGPS em um relevo plano com baixÃssima declividade e com vegetaÃÃo de porte baixo os resultados apontam um erro altimÃtrico de aproximadamente 1,7 m. A cobertura vegetal influenciou na variaÃÃo dos dados SRTM para a vegetaÃÃo com maior altura mÃdia. Para a caracterizaÃÃo fisiogrÃfica deve-se utilizar valores de Ãrea de delimitaÃÃo (threshold) que nÃo ultrapassem 50 pixels contribuintes do SRTM (90 m) necessÃrios para geraÃÃo da rede de drenagem e de um Modelo Digital de ElevaÃÃo Hidrologicamente Consistente (MDEHC) para a Ãrea de estudo. Para Ãreas com relevo plano os valores de âthresholdâ devem ser revistos. A elaboraÃÃo de um material de consulta referencial e atualizado com a caracterizaÃÃo fisiogrÃfica envolvendo o uso do Sistema de InformaÃÃes GeogrÃficas e Modelo Digital de ElevaÃÃo torna-se fundamental à medida que aumentam as possibilidades de geraÃÃo de produtos advindos do sensoriamento remoto e geoprocessamento. O uso da extensÃo ArcHydro facilita a caracterizaÃÃo fisiogrÃfica e permite o armazenamento e utilizaÃÃo destes dados como Sistema de InformaÃÃes GeogrÃficas.Conselho Nacional de Desenvolvimento CientÃfico e TecnolÃgicohttp://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=5229application/pdfinfo:eu-repo/semantics/openAccessporreponame:Biblioteca Digital de Teses e Dissertações da UFCinstname:Universidade Federal do Cearáinstacron:UFC2019-01-21T11:18:19Zmail@mail.com -
dc.title.en.fl_str_mv Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment
dc.title.alternative.pt.fl_str_mv AvaliaÃÃo dos dados SRTM atravÃs de anÃlise altimÃtrica e morfomÃtrica de bacias hidrogrÃficas no Semi-Ãrido.
title Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment
spellingShingle Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment
Carlos Alexandre Gomes Costa
IRRIGACAO E DRENAGEM
title_short Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment
title_full Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment
title_fullStr Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment
title_full_unstemmed Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment
title_sort Assessment of SRTM data by altimetric and morphometric analysis of watersheds in a semi-arid environment
author Carlos Alexandre Gomes Costa
author_facet Carlos Alexandre Gomes Costa
author_role author
dc.contributor.advisor1.fl_str_mv Adunias dos Santos Teixeira
dc.contributor.advisor1ID.fl_str_mv 33344423453
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/9646492923898649
dc.contributor.referee1.fl_str_mv Eunice Maia de Andrade
dc.contributor.referee1ID.fl_str_mv 11748729349
dc.contributor.referee1Lattes.fl_str_mv http://lattes.cnpq.br/7012348447122522
dc.contributor.referee2.fl_str_mv Marco AurÃlio Holanda de Castro
dc.contributor.referee2ID.fl_str_mv 27958892187
dc.contributor.authorID.fl_str_mv 75153033368
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/9346087418658759
dc.contributor.author.fl_str_mv Carlos Alexandre Gomes Costa
contributor_str_mv Adunias dos Santos Teixeira
Eunice Maia de Andrade
Marco AurÃlio Holanda de Castro
dc.subject.cnpq.fl_str_mv IRRIGACAO E DRENAGEM
topic IRRIGACAO E DRENAGEM
dc.description.sponsorship.fl_txt_mv Conselho Nacional de Desenvolvimento CientÃfico e TecnolÃgico
dc.description.abstract.por.fl_txt_mv Face to global climate change it is necessary a better understanding of the hydrological and environmental dynamics. To characterize them in a short time with reliability is an important requirement for the science. Topography is a major factor to understand these factors. Its determination is onerous, both economically and temporally, and the dynamics of environmental transformations that alters its pattern must be considered. In the year 2000, through a interferometric RADAR topographic mission (SRTM) led by NASA in cooperation with the German (DRL) and the Italian (ASI) space agencies, a Digital Elevation Model was generated by the employment of RADAR interferometry. These data are available costless and have been greatly used by scientists. Nonetheless, since it is a RADAR interferometer product, it represents the Earth surface and is subjected to the influence of vegetation, what may make this DEM unriliable in works that require a high detail level and good precision. Therefore, the objective of this research is to validate SRTM data to the Brazilian semi-arid conditions and, based on these data, characterize the physiograph of watersheds in the Jaguaribe basin. The methodology used in the SRTM data validation consists in a comparison and statistical analysis of field data obtained with a differential GPS (DGPS) and other data bases such as the DSG/SUDENE maps and level reference points from IBGE in the Jaguaribe basin located in Cearà State. Results present an elevation error of approximately 7 m in relation to the level reference points in the basin. For the use of DGPS on a plan relief with very low slopes and vegetation with low heights, results show an elevation error of approximately 1.7 m. Vegetation cover influenced the variation in SRTM data to vegetation with higher mean height. To the physiographic characterization, values not larger than 50 pixels must be adopted as the contributing area of SRTM (90m), used in the generation of the river network and the Hydrological Consistent Digital Elevation Model (HCDEM) in the study area. To areas with low slopes, the threshold value must be reviewed. The development of a reference bibliography with physiographic characterization associated to the use of a Geographic Information System (GIS) and a DEM is fundamental as it enhances the possibilities of generating products from remote sensing and geo-processing techniques. The use of ArcHydro extension facilitates a physiographic characterization and allows the storage and use of these data as a GIS.
Em tempos de mudanÃas globais torna-se necessÃrio cada vez mais entender a dinÃmica hidrolÃgica e ambiental. CaracterizÃ-las em um menor tempo possÃvel, com maior confiabilidade à a exigÃncia imperativa que pesa sobre a ciÃncia. A topografia evidencia-se como um fator imprescindÃvel no entendimento destes processos. Sua determinaÃÃo à onerosa, tanto economicamente quanto temporalmente, tendo ainda que considerar a dinÃmica das transformaÃÃes ambientais que alteram continuamente essa topografia.. Em 2000 atravÃs da missÃo topogrÃfica por RADAR interferomÃtrico (SRTM), liderada pela NASA com a colaboraÃÃo das agÃncias espaciais alemà (DRL) e italiana (ASI) foi gerado um Modelo Digital de ElevaÃÃo (MDE) utilizando a interferometria de RADAR. Esses dados sÃo disponÃveis gratuitamente e estÃo sendo usados em grande escala no meio cientÃfico. Entretanto, por ser um produto interferometria de RADAR, retrata a superfÃcie da terra, sofrendo inclusive a influÃncia da vegetaÃÃo, o que pode inviabilizar o uso desse MDE em trabalhos que exijam maior nÃvel de detalhamento e precisÃo.. Assim, o objetivo deste trabalho foi validar os dados SRTM para as condiÃÃes do semi-Ãrido brasileiro e a partir destes dados estimar com maior consistÃncia a caracterizaÃÃo fisiogrÃfica de bacias hidrogrÃficas afluentes do rio Jaguaribe. A metodologia utilizada na validaÃÃo dos dados SRTM consiste em comparaÃÃes e anÃlise estatÃstica com dados obtidos no campo com GPS diferencial (DGPS) e outras bases de dados referenciais existentes, cartas planialtimÃtricas DSG/ SUDENE e dados de RN do IBGE para a Bacia do Jaguaribe situada no semi-Ãrido cearense. Os resultados apresentam um erro altimÃtrico de aproximadamente 7 m com relaÃÃo aos RNs da bacia. Com uso do DGPS em um relevo plano com baixÃssima declividade e com vegetaÃÃo de porte baixo os resultados apontam um erro altimÃtrico de aproximadamente 1,7 m. A cobertura vegetal influenciou na variaÃÃo dos dados SRTM para a vegetaÃÃo com maior altura mÃdia. Para a caracterizaÃÃo fisiogrÃfica deve-se utilizar valores de Ãrea de delimitaÃÃo (threshold) que nÃo ultrapassem 50 pixels contribuintes do SRTM (90 m) necessÃrios para geraÃÃo da rede de drenagem e de um Modelo Digital de ElevaÃÃo Hidrologicamente Consistente (MDEHC) para a Ãrea de estudo. Para Ãreas com relevo plano os valores de âthresholdâ devem ser revistos. A elaboraÃÃo de um material de consulta referencial e atualizado com a caracterizaÃÃo fisiogrÃfica envolvendo o uso do Sistema de InformaÃÃes GeogrÃficas e Modelo Digital de ElevaÃÃo torna-se fundamental à medida que aumentam as possibilidades de geraÃÃo de produtos advindos do sensoriamento remoto e geoprocessamento. O uso da extensÃo ArcHydro facilita a caracterizaÃÃo fisiogrÃfica e permite o armazenamento e utilizaÃÃo destes dados como Sistema de InformaÃÃes GeogrÃficas.
description Face to global climate change it is necessary a better understanding of the hydrological and environmental dynamics. To characterize them in a short time with reliability is an important requirement for the science. Topography is a major factor to understand these factors. Its determination is onerous, both economically and temporally, and the dynamics of environmental transformations that alters its pattern must be considered. In the year 2000, through a interferometric RADAR topographic mission (SRTM) led by NASA in cooperation with the German (DRL) and the Italian (ASI) space agencies, a Digital Elevation Model was generated by the employment of RADAR interferometry. These data are available costless and have been greatly used by scientists. Nonetheless, since it is a RADAR interferometer product, it represents the Earth surface and is subjected to the influence of vegetation, what may make this DEM unriliable in works that require a high detail level and good precision. Therefore, the objective of this research is to validate SRTM data to the Brazilian semi-arid conditions and, based on these data, characterize the physiograph of watersheds in the Jaguaribe basin. The methodology used in the SRTM data validation consists in a comparison and statistical analysis of field data obtained with a differential GPS (DGPS) and other data bases such as the DSG/SUDENE maps and level reference points from IBGE in the Jaguaribe basin located in Cearà State. Results present an elevation error of approximately 7 m in relation to the level reference points in the basin. For the use of DGPS on a plan relief with very low slopes and vegetation with low heights, results show an elevation error of approximately 1.7 m. Vegetation cover influenced the variation in SRTM data to vegetation with higher mean height. To the physiographic characterization, values not larger than 50 pixels must be adopted as the contributing area of SRTM (90m), used in the generation of the river network and the Hydrological Consistent Digital Elevation Model (HCDEM) in the study area. To areas with low slopes, the threshold value must be reviewed. The development of a reference bibliography with physiographic characterization associated to the use of a Geographic Information System (GIS) and a DEM is fundamental as it enhances the possibilities of generating products from remote sensing and geo-processing techniques. The use of ArcHydro extension facilitates a physiographic characterization and allows the storage and use of these data as a GIS.
publishDate 2008
dc.date.issued.fl_str_mv 2008-03-28
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
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format masterThesis
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dc.publisher.none.fl_str_mv Universidade Federal do CearÃ
dc.publisher.program.fl_str_mv Programa de PÃs-GraduaÃÃo em Engenharia AgrÃcola
dc.publisher.initials.fl_str_mv UFC
dc.publisher.country.fl_str_mv BR
publisher.none.fl_str_mv Universidade Federal do CearÃ
dc.source.none.fl_str_mv reponame:Biblioteca Digital de Teses e Dissertações da UFC
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