2014
DOI: 10.1007/s12665-014-3869-2
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Regional and local topography subdivision and landform mapping using SRTM-derived data: a case study in southeastern Brazil

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Cited by 14 publications
(9 citation statements)
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“…The applications using the widespread free distribution DEM have gained great importance, especially among academic activities, given the wide range of possible applications, such as mapping hilltops environmental protected areas (Oliveira 2015), monitoring forest biomass (Solberg et al 2010), hydrological modeling (Ludwig and Schneider 2006), soil losses estimation (Fornelos and Neves 2007), aid in detecting neotectonic reactivations (Fonseca and Corrêa 2011), geomorphologic mapping (Camargo et al 2011), relief shapes classification (Manfré, Nóbrega and Quintanilha 2015), didactic resource for teaching and learning .…”
Section: Introductionmentioning
confidence: 99%
“…The applications using the widespread free distribution DEM have gained great importance, especially among academic activities, given the wide range of possible applications, such as mapping hilltops environmental protected areas (Oliveira 2015), monitoring forest biomass (Solberg et al 2010), hydrological modeling (Ludwig and Schneider 2006), soil losses estimation (Fornelos and Neves 2007), aid in detecting neotectonic reactivations (Fonseca and Corrêa 2011), geomorphologic mapping (Camargo et al 2011), relief shapes classification (Manfré, Nóbrega and Quintanilha 2015), didactic resource for teaching and learning .…”
Section: Introductionmentioning
confidence: 99%
“…Many macro landforms, such as volcanoes, mountains, hills, plains, and fans, and sub-classified landforms, such as high mountains, low plains, tablelands, and rough low hills, can be achieved through a designed classifier or object-based image analysis approach based on topographic variables derived from DEMs (Camargo et al, 2012; Drăguţ and Eisank, 2012; Iwahashi and Pike, 2007; Jasiewicz et al, 2014; Manfré et al, 2015; Prima et al, 2006; Saadat et al, 2008; Stepinski and Bagaria, 2009; Vannametee et al, 2014). In the aforementioned classifications, topographic variables, such as slope, curvature, local relief, roughness, etc., are calculated through neighborhood analysis, which only reflects the local topographic surface parameters and fails to reveal terrain structural features in the macro scale.…”
Section: Introductionmentioning
confidence: 99%
“…The scale and shape parameters of the segmentation process were defined according to the method of Dragut and Eisank (2012), wherein the shape and compactness factors were set to zero, and the scale parameter was defined according to the difference between the local variances of the objects. Thus, a scale parameter of 50 was used, which is similar to the value used in Manfré et al (2014).…”
Section: Digital Image Processingmentioning
confidence: 99%