2015
DOI: 10.1016/j.aeolia.2015.03.001
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Automated mapping of linear dunefield morphometric parameters from remotely-sensed data

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Cited by 27 publications
(37 citation statements)
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“…Table 2 shows that the unrealistic land-use types (which we have classified as "N/A") rarely exist: "paddy on flat sandy land" and "paddy on sand dunes". Until recently, the Advanced Spaceborne Thermal Emission and Reflection Radiometer Global Digital Elevation Model (ASTER GDEM) version 2, which has 30 m spacing and less than 12 m height accuracy (RMSE) [38], had been used as the highest-resolution, freely-available global elevation dataset for the spatial analysis of dune topography [39,40]. In April 2016, ALOS World 3D version 1 was released as a new global elevation dataset without [41].…”
Section: Depiction Of Local Land-use Typesmentioning
confidence: 99%
“…Table 2 shows that the unrealistic land-use types (which we have classified as "N/A") rarely exist: "paddy on flat sandy land" and "paddy on sand dunes". Until recently, the Advanced Spaceborne Thermal Emission and Reflection Radiometer Global Digital Elevation Model (ASTER GDEM) version 2, which has 30 m spacing and less than 12 m height accuracy (RMSE) [38], had been used as the highest-resolution, freely-available global elevation dataset for the spatial analysis of dune topography [39,40]. In April 2016, ALOS World 3D version 1 was released as a new global elevation dataset without [41].…”
Section: Depiction Of Local Land-use Typesmentioning
confidence: 99%
“…Within the aeolian analysis environment these used to define slip faces and other features with well-defined upper edges, and indirectly used to define valleys or interdune areas which are less distinct on all sides. Within the aeolian analysis environment these secondary bonified subfeatures, are termed defects with splits and crest ends identified as Y-junctions and terminations respectively [3,5,6,[21][22][23][24][25][26][27][28][29].…”
Section: Introductionmentioning
confidence: 99%
“…Previous examples of automatic characterization of aeolian features from remote sensing data include the monitoring of dune migration (Vermeesch and Drake, 2008;Necsoiu et al, 2009), detection and delimitation of dunes on Mars Orbiter Camera (MOC) data (Bandeira et al, 2011), and mapping and characterization of ripple patterns on Mars using HiRISE (High Resolution Imaging Science Experiment) data (Silvestro et al, 2013;. With the purpose of mapping automatically the crests of linear dunes from Landsat imagery, Telfer et al (2015) used a Sobel operator for performing edge detection. Using SAR data, the trends of dune fields on Titan were surveyed using a linear segment detection algorithm (von Gioi et al, 2012;Lucas et al, 2014).…”
Section: Introductionmentioning
confidence: 99%