The Assessment of using an Intelligent Algorithm for the Interpolation of Elevation in the DTM Generation Verwendung von Methoden der künstlichen Intelligenz zur Ableitung von Höhenmodellen
{"title":"The Assessment of using an Intelligent Algorithm for the Interpolation of Elevation in the DTM Generation Verwendung von Methoden der künstlichen Intelligenz zur Ableitung von Höhenmodellen","authors":"Hossein Bagheri, Saeed Sadeghian, Seyyed Yousef Sadjadi","doi":"10.1127/1432-8364/2014/0220","DOIUrl":null,"url":null,"abstract":"digital elevation model (DEM) (abDul-raHMaN & PilouK 2008). In other words, DEM continuously displays elevation changes of the Earth surface, which is directly proportional to the plane position (x,y) (abDul-raHMaN & PilouK 2008, cHaPlot et al. 2006, MillEr & laflaMME 1958). Initially, 3D models were created physically from plastic, sand, clay, etc. (li et al. 2004). Today, however, computers are used to display the Earth’s continuous surfaces in a digital form (HEESoM & MaHDJobi 2001). One of the most important issues in the field of digital modelling is the generation of a DEM with high quality and precision under minimum costs. To estimate a continuous surface, due to the limited number of samples and the necessity of reproducing altitude points,","PeriodicalId":56096,"journal":{"name":"Photogrammetrie Fernerkundung Geoinformation","volume":"6 1","pages":"197-208"},"PeriodicalIF":0.0000,"publicationDate":"2014-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"13","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Photogrammetrie Fernerkundung Geoinformation","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1127/1432-8364/2014/0220","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q","JCRName":"Social Sciences","Score":null,"Total":0}
引用次数: 13
Abstract
digital elevation model (DEM) (abDul-raHMaN & PilouK 2008). In other words, DEM continuously displays elevation changes of the Earth surface, which is directly proportional to the plane position (x,y) (abDul-raHMaN & PilouK 2008, cHaPlot et al. 2006, MillEr & laflaMME 1958). Initially, 3D models were created physically from plastic, sand, clay, etc. (li et al. 2004). Today, however, computers are used to display the Earth’s continuous surfaces in a digital form (HEESoM & MaHDJobi 2001). One of the most important issues in the field of digital modelling is the generation of a DEM with high quality and precision under minimum costs. To estimate a continuous surface, due to the limited number of samples and the necessity of reproducing altitude points,