Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno

Detalhes bibliográficos
Ano de defesa: 2015
Autor(a) principal: Ribeiro, Hugo José lattes
Orientador(a): Ferreira, Nilson Clementino lattes
Banca de defesa: Ferreira, Nilson Clementino, Milograna, Jussanã, Araújo, José Vicente Granato de, Boggione, Giovanni de Araújo
Tipo de documento: Dissertação
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal de Goiás
Programa de Pós-Graduação: Programa de Pós-graduação em Engenharia do Meio Ambiente (EEC)
Departamento: Escola de Engenharia Civil - EEC (RG)
País: Brasil
Palavras-chave em Português:
Palavras-chave em Inglês:
Área do conhecimento CNPq:
Link de acesso: http://repositorio.bc.ufg.br/tede/handle/tede/4473
Resumo: In the digital relief is best represented by the digital terrain model (DTM) and the automatic extraction from topographical parameters of this data type, configures a viable alternative in relation to the manual process performed on topographic maps. However, the available data may contain faults or present information to altitude that are not exactly the terrain. In this sense, it is important to consider these issues in the application of MDT. In hydrology, for example, you must perform preprocessing steps to eliminate inconsistencies that might prevent the natural reproduction of the flow of water toward the riverbeds. The objective of this research is to check the limits of applicability of the MDTs in hydrological analyses. For this, we used 5 (five) MDTs data: Light Detection And Ranging-LIDAR; Aerial Photography; Topodata; ASTER Global Digital Elevation Model-Aster GDEM; Shuttle Radar Topography Mission-SRTM, with different spatial resolutions and methods of acquisition. These data were applied a technique of hydrological correction and subsequently were extracted attributes from all surfaces. This information was used in the construction of the time of concentration and consequently the design hydrographs, which in turn were used to extract the maximum flow of project to return periods of 5, 10, 15, 20, 25, 50 and 100 years, in a range of the curve number (CN) varying between 40 and 99. It was built using a programming language of 60 dimension array rows by 7 columns, where each line represents the maximum values of each design hydrograph flow generated from each value of CN. In the end, it was obtained a set of 24 arrays containing the values of the maximum flows of project for each CN value, and attributes extracted of the MDTs and of digital models of terrain Hidrologicamente Consistent (MDEHCs). In possession of this information, a statistical test was applied in order to assess the influence that the hydrological consistency method and the dimensions of the cells of the MDTs/MDEHCs had about the project flows. Was observed in one of the sub-basins analysed that the difference between the maximum design flow is directly proportional to the increase in CN and payback period. It was noted a difference of up to 173.7 m3/s to a CN of 99 and return period of 100 years. The hypothesis H0 of the proposed test was accepted in all return periods both in relation to hydrological consistency method applied as compared to cell dimension of MDTs. This means that it is possible to affirm with an error probability of "P-value" for return period, which the flows generated from the parameters of the MDTs differ from flows generated from the parameters of MDEHCs as well as between the MDTs surveyed at a significance level of 5%. From the results, it might be concluded that the interpolation method for hydrological consistency and size of the cell of the MDTs has influence on the generation of the maximum flow of project.
id UFG_50d9630e9e691c73f5ac588f9bc57c9a
oai_identifier_str oai:repositorio.bc.ufg.br:tede/4473
network_acronym_str UFG
network_name_str Biblioteca Digital de Teses e Dissertações da UFG
repository_id_str
spelling Ferreira, Nilson Clementinohttp://lattes.cnpq.br/6466969611652630Milograna, JussanãFerreira, Nilson ClementinoMilograna, JussanãAraújo, José Vicente Granato deBoggione, Giovanni de Araújohttp://lattes.cnpq.br/9999213878472864Ribeiro, Hugo José2015-04-28T17:53:14Z2015-02-20RIBEIRO, H. J. Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno. 2015. 149 f. Dissertação (Mestrado em Engenharia do Meio Ambiente) - Universidade Federal de Goiás, Goiânia, 2015.http://repositorio.bc.ufg.br/tede/handle/tede/4473In the digital relief is best represented by the digital terrain model (DTM) and the automatic extraction from topographical parameters of this data type, configures a viable alternative in relation to the manual process performed on topographic maps. However, the available data may contain faults or present information to altitude that are not exactly the terrain. In this sense, it is important to consider these issues in the application of MDT. In hydrology, for example, you must perform preprocessing steps to eliminate inconsistencies that might prevent the natural reproduction of the flow of water toward the riverbeds. The objective of this research is to check the limits of applicability of the MDTs in hydrological analyses. For this, we used 5 (five) MDTs data: Light Detection And Ranging-LIDAR; Aerial Photography; Topodata; ASTER Global Digital Elevation Model-Aster GDEM; Shuttle Radar Topography Mission-SRTM, with different spatial resolutions and methods of acquisition. These data were applied a technique of hydrological correction and subsequently were extracted attributes from all surfaces. This information was used in the construction of the time of concentration and consequently the design hydrographs, which in turn were used to extract the maximum flow of project to return periods of 5, 10, 15, 20, 25, 50 and 100 years, in a range of the curve number (CN) varying between 40 and 99. It was built using a programming language of 60 dimension array rows by 7 columns, where each line represents the maximum values of each design hydrograph flow generated from each value of CN. In the end, it was obtained a set of 24 arrays containing the values of the maximum flows of project for each CN value, and attributes extracted of the MDTs and of digital models of terrain Hidrologicamente Consistent (MDEHCs). In possession of this information, a statistical test was applied in order to assess the influence that the hydrological consistency method and the dimensions of the cells of the MDTs/MDEHCs had about the project flows. Was observed in one of the sub-basins analysed that the difference between the maximum design flow is directly proportional to the increase in CN and payback period. It was noted a difference of up to 173.7 m3/s to a CN of 99 and return period of 100 years. The hypothesis H0 of the proposed test was accepted in all return periods both in relation to hydrological consistency method applied as compared to cell dimension of MDTs. This means that it is possible to affirm with an error probability of "P-value" for return period, which the flows generated from the parameters of the MDTs differ from flows generated from the parameters of MDEHCs as well as between the MDTs surveyed at a significance level of 5%. From the results, it might be concluded that the interpolation method for hydrological consistency and size of the cell of the MDTs has influence on the generation of the maximum flow of project.No meio digital o relevo é melhor representado pelo modelo digital de terreno (MDT) e, a extração automática de atributos topográficos a partir deste tipo de dado, configura-se numa alternativa viável em relação ao processo manual realizado sobre mapas topográficos. No entanto, os dados disponíveis podem conter falhas ou apresentar informações de altitude que não sejam propriamente do terreno. Neste sentido é importante considerar essas questões na aplicação do MDT. Na hidrologia, por exemplo, é preciso realizar etapas de pré-processamento para eliminar incoerências que venham impedir a reprodução natural do fluxo da água em direção aos leitos dos rios. O objetivo desta pesquisa é verificar os limites de aplicabilidade dos MDTs em análises hidrológicas. Para isto, foram utilizados 5 (cinco) dados MDTs: Light Detection And Ranging - LIDAR; Aerofotogrametria; Topodata; ASTER Global Digital Elevation Model - Aster GDEM; Shuttle Radar Topography Mission – SRTM, com diferentes resoluções espaciais e métodos de aquisição. A esses dados foi aplicada uma técnica de correção hidrológica e posteriormente foram extraídos atributos de todas as superfícies. Estas informações foram utilizadas na construção do tempo de concentração e consequentemente dos hidrogramas de projeto, que por sua vez, foram utilizados para extrair a vazão máxima de projeto para os períodos de retorno de 5, 10, 15, 20, 25, 50 e 100 anos, em uma faixa de número da curva (CN) variando entre 40 e 99. Foi construída por meio de linguagem de programação uma matriz de dimensão 60 linhas por 7 colunas, onde cada linha representa os valores máximos de vazão de cada hidrograma de projeto gerado a partir de cada valor de CN. No final obteve-se um conjunto de 24 matrizes contendo os valores de vazões máximas de projeto para cada valor de CN, além de atributos extraídos dos MDTs e dos Modelos Digitais de Terreno Hidrologicamente Consistentes (MDEHCs). De posse dessas informações foi aplicado um teste estatístico, com o intuito de avaliar a influência que o método de consistência hidrológica e as dimensões das células dos MDTs/MDEHCs tiveram sobre as vazões de projeto. Foi observado em uma das sub-bacias analisadas que a diferença entre as vazões máximas de projeto é diretamente proporcional ao aumento do CN e período de retorno. Notou-se uma diferença de até 173,7 m3/s para um CN de 99 e período de retorno de 100 anos. A hipótese H0 do teste proposto foi aceita em todos os períodos de retorno tanto em relação ao método de consistência hidrológica aplicado quanto em relação ao tamanho da célula dos MDTs. Isto significa que é possível afirmar com uma probabilidade de erro de “P-Valor” por período de retorno, que as vazões geradas a partir dos atributos dos MDTs diferem das vazões geradas a partir dos atributos dos MDEHCs, assim como, entre os MDTs pesquisados a um nível de significância de 5%. A partir dos resultados pôde-se concluir que o método de interpolação para consistência hidrológica e tamanho da célula dos MDTs tem influência sobre a geração da vazão máxima de projeto.Submitted by Erika Demachki (erikademachki@gmail.com) on 2015-04-28T17:48:29Z No. of bitstreams: 2 Dissertação - Hugo José Ribeiro - 2015.pdf: 4005712 bytes, checksum: 3ca2bfd5ce9d093857a0f4a6501f84f1 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5)Approved for entry into archive by Erika Demachki (erikademachki@gmail.com) on 2015-04-28T17:53:14Z (GMT) No. of bitstreams: 2 Dissertação - Hugo José Ribeiro - 2015.pdf: 4005712 bytes, checksum: 3ca2bfd5ce9d093857a0f4a6501f84f1 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5)Made available in DSpace on 2015-04-28T17:53:14Z (GMT). No. of bitstreams: 2 Dissertação - Hugo José Ribeiro - 2015.pdf: 4005712 bytes, checksum: 3ca2bfd5ce9d093857a0f4a6501f84f1 (MD5) license_rdf: 23148 bytes, checksum: 9da0b6dfac957114c6a7714714b86306 (MD5) Previous issue date: 2015-02-20Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPESapplication/pdfhttp://repositorio.bc.ufg.br/tede/retrieve/19317/Disserta%c3%a7%c3%a3o%20-%20Hugo%20Jos%c3%a9%20Ribeiro%20-%202015.pdf.jpgporUniversidade Federal de GoiásPrograma de Pós-graduação em Engenharia do Meio Ambiente (EEC)UFGBrasilEscola de Engenharia Civil - EEC (RG)http://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessMDEHCVazão de projetoConsistência hidrológicaTamanho da célulaDEMHCProject flowHydrological consistencyCell SizeENGENHARIASAnálise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terrenoAnalysis of hydrological data consistency a different models from land of digitalinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesis100970209197287484760060060060072408725162631558545189710564848268252075167498588264571reponame:Biblioteca Digital de Teses e Dissertações da UFGinstname:Universidade Federal de Goiás (UFG)instacron:UFGLICENSElicense.txtlicense.txttext/plain; charset=utf-82165http://repositorio.bc.ufg.br/tede/bitstreams/5b4cd7d4-b5ad-4289-b909-762609a166ce/downloadbd3efa91386c1718a7f26a329fdcb468MD51CC-LICENSElicense_urllicense_urltext/plain; charset=utf-849http://repositorio.bc.ufg.br/tede/bitstreams/fc0ea22b-2ea2-4f4a-9f95-0212a6bfbde4/download4afdbb8c545fd630ea7db775da747b2fMD52license_textlicense_texttext/html; charset=utf-822762http://repositorio.bc.ufg.br/tede/bitstreams/04f48684-b533-44ad-8bd3-da67839a93cd/downloadfda13080e892f3f68def2b8b70227968MD53license_rdflicense_rdfapplication/rdf+xml; charset=utf-823148http://repositorio.bc.ufg.br/tede/bitstreams/001980a9-af69-4124-8c5c-1acbb4ec5572/download9da0b6dfac957114c6a7714714b86306MD54ORIGINALDissertação - Hugo José Ribeiro - 2015.pdfDissertação - Hugo José Ribeiro - 2015.pdfapplication/pdf4005712http://repositorio.bc.ufg.br/tede/bitstreams/b1835826-68f3-4f40-ba29-13e277a6948e/download3ca2bfd5ce9d093857a0f4a6501f84f1MD55TEXTDissertação - Hugo José Ribeiro - 2015.pdf.txtDissertação - Hugo José Ribeiro - 2015.pdf.txtExtracted Texttext/plain312365http://repositorio.bc.ufg.br/tede/bitstreams/76dbb9a6-c483-4a32-8e11-97fcdbca91a5/downloadd184c21cbc844db15df39c66711b0478MD56THUMBNAILDissertação - Hugo José Ribeiro - 2015.pdf.jpgDissertação - Hugo José Ribeiro - 2015.pdf.jpgGenerated Thumbnailimage/jpeg1950http://repositorio.bc.ufg.br/tede/bitstreams/40159bb6-37ad-42d0-ad15-c490d30ef641/downloadc45a30836bfd6f88144a77ac1ee7f596MD57tede/44732015-04-29 03:02:13.238http://creativecommons.org/licenses/by-nc-nd/4.0/Acesso Abertoopen.accessoai:repositorio.bc.ufg.br:tede/4473http://repositorio.bc.ufg.br/tedeBiblioteca Digital de Teses e Dissertaçõeshttp://repositorio.bc.ufg.br/PUBhttps://repositorio.bc.ufg.br/tede_oai/requesttesesdissertacoes.bc@ufg.br ||tesesdissertacoes.bc@ufg.bropendoar:32082015-04-29T06:02:13Biblioteca Digital de Teses e Dissertações da UFG - Universidade Federal de Goiás (UFG)falseTk9UQTogQ09MT1FVRSBBUVVJIEEgU1VBIFBSw5NQUklBIExJQ0VOw4dBCkVzdGEgbGljZW7Dp2EgZGUgZXhlbXBsbyDDqSBmb3JuZWNpZGEgYXBlbmFzIHBhcmEgZmlucyBpbmZvcm1hdGl2b3MuCgpMSUNFTsOHQSBERSBESVNUUklCVUnDh8ODTyBOw4NPLUVYQ0xVU0lWQQoKQ29tIGEgYXByZXNlbnRhw6fDo28gZGVzdGEgbGljZW7Dp2EsIHZvY8OqIChvIGF1dG9yIChlcykgb3UgbyB0aXR1bGFyIGRvcyBkaXJlaXRvcyBkZSBhdXRvcikgY29uY2VkZSDDoCBVbml2ZXJzaWRhZGUgClhYWCAoU2lnbGEgZGEgVW5pdmVyc2lkYWRlKSBvIGRpcmVpdG8gbsOjby1leGNsdXNpdm8gZGUgcmVwcm9kdXppciwgIHRyYWR1emlyIChjb25mb3JtZSBkZWZpbmlkbyBhYmFpeG8pLCBlL291IApkaXN0cmlidWlyIGEgc3VhIHRlc2Ugb3UgZGlzc2VydGHDp8OjbyAoaW5jbHVpbmRvIG8gcmVzdW1vKSBwb3IgdG9kbyBvIG11bmRvIG5vIGZvcm1hdG8gaW1wcmVzc28gZSBlbGV0csO0bmljbyBlIAplbSBxdWFscXVlciBtZWlvLCBpbmNsdWluZG8gb3MgZm9ybWF0b3Mgw6F1ZGlvIG91IHbDrWRlby4KClZvY8OqIGNvbmNvcmRhIHF1ZSBhIFNpZ2xhIGRlIFVuaXZlcnNpZGFkZSBwb2RlLCBzZW0gYWx0ZXJhciBvIGNvbnRlw7pkbywgdHJhbnNwb3IgYSBzdWEgdGVzZSBvdSBkaXNzZXJ0YcOnw6NvIApwYXJhIHF1YWxxdWVyIG1laW8gb3UgZm9ybWF0byBwYXJhIGZpbnMgZGUgcHJlc2VydmHDp8Ojby4KClZvY8OqIHRhbWLDqW0gY29uY29yZGEgcXVlIGEgU2lnbGEgZGUgVW5pdmVyc2lkYWRlIHBvZGUgbWFudGVyIG1haXMgZGUgdW1hIGPDs3BpYSBhIHN1YSB0ZXNlIG91IApkaXNzZXJ0YcOnw6NvIHBhcmEgZmlucyBkZSBzZWd1cmFuw6dhLCBiYWNrLXVwIGUgcHJlc2VydmHDp8Ojby4KClZvY8OqIGRlY2xhcmEgcXVlIGEgc3VhIHRlc2Ugb3UgZGlzc2VydGHDp8OjbyDDqSBvcmlnaW5hbCBlIHF1ZSB2b2PDqiB0ZW0gbyBwb2RlciBkZSBjb25jZWRlciBvcyBkaXJlaXRvcyBjb250aWRvcyAKbmVzdGEgbGljZW7Dp2EuIFZvY8OqIHRhbWLDqW0gZGVjbGFyYSBxdWUgbyBkZXDDs3NpdG8gZGEgc3VhIHRlc2Ugb3UgZGlzc2VydGHDp8OjbyBuw6NvLCBxdWUgc2VqYSBkZSBzZXUgCmNvbmhlY2ltZW50bywgaW5mcmluZ2UgZGlyZWl0b3MgYXV0b3JhaXMgZGUgbmluZ3XDqW0uCgpDYXNvIGEgc3VhIHRlc2Ugb3UgZGlzc2VydGHDp8OjbyBjb250ZW5oYSBtYXRlcmlhbCBxdWUgdm9jw6ogbsOjbyBwb3NzdWkgYSB0aXR1bGFyaWRhZGUgZG9zIGRpcmVpdG9zIGF1dG9yYWlzLCB2b2PDqiAKZGVjbGFyYSBxdWUgb2J0ZXZlIGEgcGVybWlzc8OjbyBpcnJlc3RyaXRhIGRvIGRldGVudG9yIGRvcyBkaXJlaXRvcyBhdXRvcmFpcyBwYXJhIGNvbmNlZGVyIMOgIFNpZ2xhIGRlIFVuaXZlcnNpZGFkZSAKb3MgZGlyZWl0b3MgYXByZXNlbnRhZG9zIG5lc3RhIGxpY2Vuw6dhLCBlIHF1ZSBlc3NlIG1hdGVyaWFsIGRlIHByb3ByaWVkYWRlIGRlIHRlcmNlaXJvcyBlc3TDoSBjbGFyYW1lbnRlIAppZGVudGlmaWNhZG8gZSByZWNvbmhlY2lkbyBubyB0ZXh0byBvdSBubyBjb250ZcO6ZG8gZGEgdGVzZSBvdSBkaXNzZXJ0YcOnw6NvIG9yYSBkZXBvc2l0YWRhLgoKQ0FTTyBBIFRFU0UgT1UgRElTU0VSVEHDh8ODTyBPUkEgREVQT1NJVEFEQSBURU5IQSBTSURPIFJFU1VMVEFETyBERSBVTSBQQVRST0PDjU5JTyBPVSAKQVBPSU8gREUgVU1BIEFHw4pOQ0lBIERFIEZPTUVOVE8gT1UgT1VUUk8gT1JHQU5JU01PIFFVRSBOw4NPIFNFSkEgQSBTSUdMQSBERSAKVU5JVkVSU0lEQURFLCBWT0PDiiBERUNMQVJBIFFVRSBSRVNQRUlUT1UgVE9ET1MgRSBRVUFJU1FVRVIgRElSRUlUT1MgREUgUkVWSVPDg08gQ09NTyAKVEFNQsOJTSBBUyBERU1BSVMgT0JSSUdBw4fDlUVTIEVYSUdJREFTIFBPUiBDT05UUkFUTyBPVSBBQ09SRE8uCgpBIFNpZ2xhIGRlIFVuaXZlcnNpZGFkZSBzZSBjb21wcm9tZXRlIGEgaWRlbnRpZmljYXIgY2xhcmFtZW50ZSBvIHNldSBub21lIChzKSBvdSBvKHMpIG5vbWUocykgZG8ocykgCmRldGVudG9yKGVzKSBkb3MgZGlyZWl0b3MgYXV0b3JhaXMgZGEgdGVzZSBvdSBkaXNzZXJ0YcOnw6NvLCBlIG7Do28gZmFyw6EgcXVhbHF1ZXIgYWx0ZXJhw6fDo28sIGFsw6ltIGRhcXVlbGFzIApjb25jZWRpZGFzIHBvciBlc3RhIGxpY2Vuw6dhLgo=
dc.title.por.fl_str_mv Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno
dc.title.alternative.eng.fl_str_mv Analysis of hydrological data consistency a different models from land of digital
title Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno
spellingShingle Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno
Ribeiro, Hugo José
MDEHC
Vazão de projeto
Consistência hidrológica
Tamanho da célula
DEMHC
Project flow
Hydrological consistency
Cell Size
ENGENHARIAS
title_short Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno
title_full Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno
title_fullStr Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno
title_full_unstemmed Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno
title_sort Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno
author Ribeiro, Hugo José
author_facet Ribeiro, Hugo José
author_role author
dc.contributor.advisor1.fl_str_mv Ferreira, Nilson Clementino
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/6466969611652630
dc.contributor.advisor-co1.fl_str_mv Milograna, Jussanã
dc.contributor.referee1.fl_str_mv Ferreira, Nilson Clementino
dc.contributor.referee2.fl_str_mv Milograna, Jussanã
dc.contributor.referee3.fl_str_mv Araújo, José Vicente Granato de
dc.contributor.referee4.fl_str_mv Boggione, Giovanni de Araújo
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/9999213878472864
dc.contributor.author.fl_str_mv Ribeiro, Hugo José
contributor_str_mv Ferreira, Nilson Clementino
Milograna, Jussanã
Ferreira, Nilson Clementino
Milograna, Jussanã
Araújo, José Vicente Granato de
Boggione, Giovanni de Araújo
dc.subject.por.fl_str_mv MDEHC
Vazão de projeto
Consistência hidrológica
Tamanho da célula
topic MDEHC
Vazão de projeto
Consistência hidrológica
Tamanho da célula
DEMHC
Project flow
Hydrological consistency
Cell Size
ENGENHARIAS
dc.subject.eng.fl_str_mv DEMHC
Project flow
Hydrological consistency
Cell Size
dc.subject.cnpq.fl_str_mv ENGENHARIAS
description In the digital relief is best represented by the digital terrain model (DTM) and the automatic extraction from topographical parameters of this data type, configures a viable alternative in relation to the manual process performed on topographic maps. However, the available data may contain faults or present information to altitude that are not exactly the terrain. In this sense, it is important to consider these issues in the application of MDT. In hydrology, for example, you must perform preprocessing steps to eliminate inconsistencies that might prevent the natural reproduction of the flow of water toward the riverbeds. The objective of this research is to check the limits of applicability of the MDTs in hydrological analyses. For this, we used 5 (five) MDTs data: Light Detection And Ranging-LIDAR; Aerial Photography; Topodata; ASTER Global Digital Elevation Model-Aster GDEM; Shuttle Radar Topography Mission-SRTM, with different spatial resolutions and methods of acquisition. These data were applied a technique of hydrological correction and subsequently were extracted attributes from all surfaces. This information was used in the construction of the time of concentration and consequently the design hydrographs, which in turn were used to extract the maximum flow of project to return periods of 5, 10, 15, 20, 25, 50 and 100 years, in a range of the curve number (CN) varying between 40 and 99. It was built using a programming language of 60 dimension array rows by 7 columns, where each line represents the maximum values of each design hydrograph flow generated from each value of CN. In the end, it was obtained a set of 24 arrays containing the values of the maximum flows of project for each CN value, and attributes extracted of the MDTs and of digital models of terrain Hidrologicamente Consistent (MDEHCs). In possession of this information, a statistical test was applied in order to assess the influence that the hydrological consistency method and the dimensions of the cells of the MDTs/MDEHCs had about the project flows. Was observed in one of the sub-basins analysed that the difference between the maximum design flow is directly proportional to the increase in CN and payback period. It was noted a difference of up to 173.7 m3/s to a CN of 99 and return period of 100 years. The hypothesis H0 of the proposed test was accepted in all return periods both in relation to hydrological consistency method applied as compared to cell dimension of MDTs. This means that it is possible to affirm with an error probability of "P-value" for return period, which the flows generated from the parameters of the MDTs differ from flows generated from the parameters of MDEHCs as well as between the MDTs surveyed at a significance level of 5%. From the results, it might be concluded that the interpolation method for hydrological consistency and size of the cell of the MDTs has influence on the generation of the maximum flow of project.
publishDate 2015
dc.date.accessioned.fl_str_mv 2015-04-28T17:53:14Z
dc.date.issued.fl_str_mv 2015-02-20
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
format masterThesis
status_str publishedVersion
dc.identifier.citation.fl_str_mv RIBEIRO, H. J. Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno. 2015. 149 f. Dissertação (Mestrado em Engenharia do Meio Ambiente) - Universidade Federal de Goiás, Goiânia, 2015.
dc.identifier.uri.fl_str_mv http://repositorio.bc.ufg.br/tede/handle/tede/4473
identifier_str_mv RIBEIRO, H. J. Análise da consistência de dados hidrológicos a partir de diferentes modelos digitais de terreno. 2015. 149 f. Dissertação (Mestrado em Engenharia do Meio Ambiente) - Universidade Federal de Goiás, Goiânia, 2015.
url http://repositorio.bc.ufg.br/tede/handle/tede/4473
dc.language.iso.fl_str_mv por
language por
dc.relation.program.fl_str_mv 1009702091972874847
dc.relation.confidence.fl_str_mv 600
600
600
600
dc.relation.department.fl_str_mv 724087251626315585
dc.relation.cnpq.fl_str_mv 4518971056484826825
dc.relation.sponsorship.fl_str_mv 2075167498588264571
dc.rights.driver.fl_str_mv http://creativecommons.org/licenses/by-nc-nd/4.0/
info:eu-repo/semantics/openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-nd/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal de Goiás
dc.publisher.program.fl_str_mv Programa de Pós-graduação em Engenharia do Meio Ambiente (EEC)
dc.publisher.initials.fl_str_mv UFG
dc.publisher.country.fl_str_mv Brasil
dc.publisher.department.fl_str_mv Escola de Engenharia Civil - EEC (RG)
publisher.none.fl_str_mv Universidade Federal de Goiás
dc.source.none.fl_str_mv reponame:Biblioteca Digital de Teses e Dissertações da UFG
instname:Universidade Federal de Goiás (UFG)
instacron:UFG
instname_str Universidade Federal de Goiás (UFG)
instacron_str UFG
institution UFG
reponame_str Biblioteca Digital de Teses e Dissertações da UFG
collection Biblioteca Digital de Teses e Dissertações da UFG
bitstream.url.fl_str_mv http://repositorio.bc.ufg.br/tede/bitstreams/5b4cd7d4-b5ad-4289-b909-762609a166ce/download
http://repositorio.bc.ufg.br/tede/bitstreams/fc0ea22b-2ea2-4f4a-9f95-0212a6bfbde4/download
http://repositorio.bc.ufg.br/tede/bitstreams/04f48684-b533-44ad-8bd3-da67839a93cd/download
http://repositorio.bc.ufg.br/tede/bitstreams/001980a9-af69-4124-8c5c-1acbb4ec5572/download
http://repositorio.bc.ufg.br/tede/bitstreams/b1835826-68f3-4f40-ba29-13e277a6948e/download
http://repositorio.bc.ufg.br/tede/bitstreams/76dbb9a6-c483-4a32-8e11-97fcdbca91a5/download
http://repositorio.bc.ufg.br/tede/bitstreams/40159bb6-37ad-42d0-ad15-c490d30ef641/download
bitstream.checksum.fl_str_mv bd3efa91386c1718a7f26a329fdcb468
4afdbb8c545fd630ea7db775da747b2f
fda13080e892f3f68def2b8b70227968
9da0b6dfac957114c6a7714714b86306
3ca2bfd5ce9d093857a0f4a6501f84f1
d184c21cbc844db15df39c66711b0478
c45a30836bfd6f88144a77ac1ee7f596
bitstream.checksumAlgorithm.fl_str_mv MD5
MD5
MD5
MD5
MD5
MD5
MD5
repository.name.fl_str_mv Biblioteca Digital de Teses e Dissertações da UFG - Universidade Federal de Goiás (UFG)
repository.mail.fl_str_mv tesesdissertacoes.bc@ufg.br ||tesesdissertacoes.bc@ufg.br
_version_ 1797047705327894528