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  • Evolution of the lowest amazon basin modeled from the integration of geological and SRTM topographic data
  • Morphologic features obtained from Shuttle Radar Topographic Mission (SRTM) data, integrated with geologic information, are emphasized in this paper in order to provide the basis for understanding the development of the lowest Amazon drainage basin
  • Soil parent material delineation using MODIS and SRTM data
  • The aim of the study was to develop a robust, remote sensing (MODIS and SRTM) based procedure to delineate soil parent material (PM) classes for small scale soil mapping applications. This quantitative procedure aimed to maintain the original
  • and thermal channels were used to compile the RS dataset which was later complemented with SRTM data and terrain derivatives as well. - (AM)
  • A comparison of SRTM and high-resolution digital elevation models and their use in catchment geomorphology and hydrology : Australian examples
  • The AA. examine the Shuttle Radar Topography Mission (STRM) data for 3 catchments in Australia over a range of climates, geology and resultant geomorphology. The SRTM data are compared with high resolution digital elevation models. The AA. use basic
  • hydrology and geomorphology, as in all cases SRTM-derived catchment area is incorrect and smaller digital elevation grid sizes are required for accurate catchment-wide assessment.
  • Photo-interprétation du modèle numérique de terrain SRTM, pour l'étude des directions privilégiées de percolation (site de Bursa, Turquie)
  • spatiale des données altimétriques SRTM et ainsi obtenir la localisation des fractures majeures de surface et leurs caractérisations théoriques par photo-interprétation. Enfin, ils présentent les résultats de l'analyse hydrogéologique de la région de Bursa
  • A geomorphometric analysis of Poland on the basis of SRTM-3 data
  • Analyse quantitative ; Carte géomorphologique ; Géomorphométrie ; Hypsométrie ; Image satellite ; Pente de versant ; Pologne ; Relief ; SRTM ; Topographie ; Traitement des données ; Télédétection
  • fields. Maps of hypsometry, elevation difference, angle of slope, exposure and standard deviation were also presented. The survey involved elevation data from the SRTM-3 satellite with a resolution of 3×3' (60-65×90 m), which were converted for research
  • Investigation of elevation bias of the SRTM C- and X-band digital elevation models
  • Réduction du chatoiement et apport des données ASAR ENVISAT et MNE SRTM à la cartographie hydrostructurale du bassin côtier de l'Agnéby (Sud-Est de la Côte d'Ivoire)
  • images ASAR/ENVISAT et du modèle numérique d'élévation (MNE) de la campagne SRTM s'est révélé très pertinent pour la cartographie hydrostructurale du bassin de l'Agnéby. La synthèse des structures géologiques interprétées a permis de disposer d'une base
  • Satellite imageries from Landsat ETM+ and ERS (European Remote Sensing) Radar sensors, together with elevation data collected by the Shuttle Radar Topography Mission (SRTM) in addition to recent and older bibliography, have led to the hypothesis
  • Post-1930 directions to land-use changes in the Polish-Slovakian border region of the Małe Pieniny Mts. are presented, on the basis of research concerning archival topographic maps, contemporary panchromatic satellite data and an SRTM digital
  • remote sensing, field survey and historical sources were correlated and correction factors established; the SRTM was found to be partly unsuitable for further assessments. Further analysis of remote sensing data was used to investigate the Sudd's inland
  • (Medves and Völgység) using spatial database and GIS. Slope, soil and land cover parameters were combined to create erosion risk maps. The SRTM, the CORINE land cover database and the Hungarian agro-topographical database, the AGROTOPO were available from
  • En premier, les AA. dressent une nouvelle carte géologique et structurale des structures plissées de la région de Métlaoui à partir de l'analyse d'images Landsat 5 et 7 drapées sur un modèle numérique de terrain SRTM. Cette cartographie en 2,5-D
  • of this once homogeneous surface. GIS-based statistical methods have been used by authors to calculate exact aspects and slopes of the relict surfaces using the Shuttle Radar Topography Mission digital terrain model (SRTM DTM). - (AM)
  • with estimates from laboratory analysis of field samples. The results suggest that palaeo-lake highstands, reconstructed here using the SRTM 3 arc-second digital elevation model, have left behind surficial carbonate deposits, which can be mapped by the MODIS
  • to the population product include MODIS landcover, SRTM topography and high-resolution imagery. Calibration of the global constructed area density product was derived from high-resolution aerial photographs. The AA. demonstrate that a satellite derived constructed
  • This work presents the results of a quantitative analysis of an interferometric SAR (InSAR) digital elevation model (DEM), obtained by the Shuttle Radar Topography Mission (SRTM). The analysis aims to identify additional parameters to recognize
  • hêtraies de l'Institut forestier national (IFN), un modèle numérique de terrain (MNT, SRTM) et quatre indices de vulnérabilité du hêtre identifiés dans la littérature. La méthode repose sur une interpolation fine (mailles de 100 m) de ces indices par
  • is calculated using the meteorological data released by WorldClim and mountain base elevation (as a proxy of mass elevation effect) is extracted on the basis of SRTM 90-meter resolution elevation data. The results show that MEE is simply the primary factor
  • et du modèle numérique de terrain SRTM, l’A. fait une représentation du réseau de drainage et le compare ensuite avec celui obtenu grâce aux données topographiques. Elle met en évidence les conditions de la formation du réseau de drainage à la surface
  • m), ASTER DEM (15 m) and GDEM (30 m), and SRTM (90 m). The example shows that (apart from the LiDAR) the NED10, which is generated from composite data sources, is the least error-ridden DEM for that region. Knowing error magnitudes and where errors