DOI: 10.11606/t.18.2011.tde-19122011-144406
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Estimativa do escorrimento superficial e da produção de sedimentos em áreas de atividades agrossilvopastoris, no Estado de São Paulo, em função da mudança de uso e cobertura do solo

Abstract: Baca, pesquisador da Embrapa Solos pela confiança e disponibilização de dados necessários para essa pesquisa. Ao Dr. Peter Verburg e à Universidade de Wageningen, por disponibilizar o modelo de simulação CLUES , fundamental para a execução desse trabalho.

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“…Daily maximum and minimum temperatures, wind speed, humidity and insolation were obtained from the National Meteorological Institute [112] and from one station at the University of São Paulo [113] ( Figure 4-2), while missing data was generated in SWAT based on monthly statistics created from long-term measured available data. Solar radiation values were estimated based on insolation from the weather station network [114,115,116] .…”
Section: -33 Model Setup and Data Setsmentioning
confidence: 99%
“…Daily maximum and minimum temperatures, wind speed, humidity and insolation were obtained from the National Meteorological Institute [112] and from one station at the University of São Paulo [113] ( Figure 4-2), while missing data was generated in SWAT based on monthly statistics created from long-term measured available data. Solar radiation values were estimated based on insolation from the weather station network [114,115,116] .…”
Section: -33 Model Setup and Data Setsmentioning
confidence: 99%
“…O CLUE-S corresponde a um aprimoramento da aplicabilidade do CLUE para um nível de análise regional e local, ou seja, de maior resolução espacial (VERBUG et al, 2002;SOLER, 2010;GALHARTE, 2011;PEREIRA, 2013 (SILVA Júnior. et al, 2003;PRUSKI et al, 2012).…”
Section: Modelagem Dinâmica Utilizando O Modelo Clue-s (Conversion Ofunclassified
“…Para isso, têm-se buscado aplicar diferentes técnicas para medir e estimar a evapotranspiração potencial e real, sendo que esses resultados tem sido semelhantes aos encontrados no presente trabalho (DUFRENE et al, 1993;KALLARACKAL et al, 2004;YUSOP et al, 2008;CARR, 2011;BAKOUME et al, 2013;ARSHAD, 2014;MEIJIDE et al, 2015;. VERBURG et al, 2002;KUHN, 2005;VERBURG et al, 2006b;VALENCIA, 2008, SOLER et al, 2009LUO et al, 2010;GALHARTE, 2011;PEREIRA, 2013) Figuras 65: Mapas de distância euclidiana e logarítmica a hidrografias para as sub-bacias dos rios Bujaru e Mariquita.…”
Section: D) Balanço Hídrico No Exultório Das Sub-bacias Não Monitoradunclassified