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Modification of a digital elevation model (DEM) in a flat topographic area with respect to manmade features
This study compares two Digital Elevation Models (DEMs) that are available free of charge: (1) the Consultative Group for International Agriculture Research Consortium for Spatial Information SRTM C-band CGIAR-CSI v4.1 (SRTM): 3 arc sec (approximately 92 m at the equator; originally 1 arc sec but on...
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Published in: | Geosciences journal (Seoul, Korea) 2016, 20(1), , pp.101-115 |
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description | This study compares two Digital Elevation Models (DEMs) that are available free of charge: (1) the Consultative Group for International Agriculture Research Consortium for Spatial Information SRTM C-band CGIAR-CSI v4.1 (SRTM): 3 arc sec (approximately 92 m at the equator; originally 1 arc sec but only distributed with 3 arc sec) and (2) the Advanced Spaceborne Thermal Emission and Reflection Radiometer-Global Digital Elevation Model ASTER GDEM v2 (ASTER2): 1 arc sec (approximately 31 m at the equator). Additionally, the DEM was modified according to known topographic features in the study area. The first step was investigating whether there is a spatial shift between the different DEMs by using a very high resolution (VHR) satellite GeoEye image. Beside visual comparisons, statistical methods were applied to compare the elevation models. Reference data used in this study are the Ground Control Points (GCPs) collected in a previous investigation in the same study area. SRTM proved to be the better of two available free elevation models (SRTM and ASTER2). This conclusion is based on an assessment of the different investigated aspects such as morphologic details, reliability, completeness, and accuracy. The ability to modify the SRTM model with 92 m horizontal resolution from the Shuttle Radar Topography Mission is here discussed. The study area is located in Titas Upazila, Comilla district, Bangladesh and comprises manmade topographic features (e.g., road embankments and mounds that houses are built on above the monsoon flooding level), which are not or not completely represented in the DEM due to their small spatial extent. To represent these topographic features, the DEM was refined by dividing each pixel into 0.5 m pixel spacings. The elevated areas (roads and villages) were digitized using GeoEye satellite imagery and Google Earth. The pixels located in the elevated areas were given the proper elevation and rejoined to the original DEM raster. The effect of trees can be excluded because of their scarcity in the studied area, and because their existence is limited just to both sides of the artificially elevated streets and areas where people live. Furthermore, the bias in the SRTM model is eliminated by two steps: (1) the mean (value) of the differences between the GCPs and the corresponding points of the SRTM is subtracted from SRTM points, and then the root mean square error (RMSE) is diminished to 0.67 m; (2) the same mean (value) of the differences is |
doi_str_mv | 10.1007/s12303-015-0020-7 |
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Additionally, the DEM was modified according to known topographic features in the study area. The first step was investigating whether there is a spatial shift between the different DEMs by using a very high resolution (VHR) satellite GeoEye image. Beside visual comparisons, statistical methods were applied to compare the elevation models. Reference data used in this study are the Ground Control Points (GCPs) collected in a previous investigation in the same study area. SRTM proved to be the better of two available free elevation models (SRTM and ASTER2). This conclusion is based on an assessment of the different investigated aspects such as morphologic details, reliability, completeness, and accuracy. The ability to modify the SRTM model with 92 m horizontal resolution from the Shuttle Radar Topography Mission is here discussed. The study area is located in Titas Upazila, Comilla district, Bangladesh and comprises manmade topographic features (e.g., road embankments and mounds that houses are built on above the monsoon flooding level), which are not or not completely represented in the DEM due to their small spatial extent. To represent these topographic features, the DEM was refined by dividing each pixel into 0.5 m pixel spacings. The elevated areas (roads and villages) were digitized using GeoEye satellite imagery and Google Earth. The pixels located in the elevated areas were given the proper elevation and rejoined to the original DEM raster. The effect of trees can be excluded because of their scarcity in the studied area, and because their existence is limited just to both sides of the artificially elevated streets and areas where people live. Furthermore, the bias in the SRTM model is eliminated by two steps: (1) the mean (value) of the differences between the GCPs and the corresponding points of the SRTM is subtracted from SRTM points, and then the root mean square error (RMSE) is diminished to 0.67 m; (2) the same mean (value) of the differences is subtracted from the whole SRTM model. The finally modified DEM represents the real terrain surface with the most important details of the study area. This modified elevation model may be used in studies to model groundwater flow driven by topography.</description><identifier>ISSN: 1226-4806</identifier><identifier>EISSN: 1598-7477</identifier><identifier>DOI: 10.1007/s12303-015-0020-7</identifier><language>eng</language><publisher>Seoul: The Geological Society of Korea</publisher><subject>Agricultural research ; Agriculture ; Charge ; Computer based modeling ; Consultancy services ; Digital Elevation Models ; Earth and Environmental Science ; Earth Sciences ; Elevation ; Embankments ; Equator ; Groundwater flow ; Mounds ; Pixels ; Radiometry ; Roads ; Satellite imagery ; Statistical methods ; Studies ; Topography ; 지질학</subject><ispartof>Geosciences Journal, 2016, 20(1), , pp.101-115</ispartof><rights>The Association of Korean Geoscience Societies and Springer-Verlag Berlin Heidelberg 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c381t-d92be257e126c549cbe92b9770c002a478eb30a6f07e3f1c157b1ff2c6362ea03</citedby><cites>FETCH-LOGICAL-c381t-d92be257e126c549cbe92b9770c002a478eb30a6f07e3f1c157b1ff2c6362ea03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttps://www.kci.go.kr/kciportal/ci/sereArticleSearch/ciSereArtiView.kci?sereArticleSearchBean.artiId=ART002076572$$DAccess content in National Research Foundation of Korea (NRF)$$Hfree_for_read</backlink></links><search><creatorcontrib>Kanoua, Wael</creatorcontrib><creatorcontrib>Merkel, Broder J.</creatorcontrib><title>Modification of a digital elevation model (DEM) in a flat topographic area with respect to manmade features</title><title>Geosciences journal (Seoul, Korea)</title><addtitle>Geosci J</addtitle><description>This study compares two Digital Elevation Models (DEMs) that are available free of charge: (1) the Consultative Group for International Agriculture Research Consortium for Spatial Information SRTM C-band CGIAR-CSI v4.1 (SRTM): 3 arc sec (approximately 92 m at the equator; originally 1 arc sec but only distributed with 3 arc sec) and (2) the Advanced Spaceborne Thermal Emission and Reflection Radiometer-Global Digital Elevation Model ASTER GDEM v2 (ASTER2): 1 arc sec (approximately 31 m at the equator). Additionally, the DEM was modified according to known topographic features in the study area. The first step was investigating whether there is a spatial shift between the different DEMs by using a very high resolution (VHR) satellite GeoEye image. Beside visual comparisons, statistical methods were applied to compare the elevation models. Reference data used in this study are the Ground Control Points (GCPs) collected in a previous investigation in the same study area. SRTM proved to be the better of two available free elevation models (SRTM and ASTER2). This conclusion is based on an assessment of the different investigated aspects such as morphologic details, reliability, completeness, and accuracy. The ability to modify the SRTM model with 92 m horizontal resolution from the Shuttle Radar Topography Mission is here discussed. The study area is located in Titas Upazila, Comilla district, Bangladesh and comprises manmade topographic features (e.g., road embankments and mounds that houses are built on above the monsoon flooding level), which are not or not completely represented in the DEM due to their small spatial extent. To represent these topographic features, the DEM was refined by dividing each pixel into 0.5 m pixel spacings. The elevated areas (roads and villages) were digitized using GeoEye satellite imagery and Google Earth. The pixels located in the elevated areas were given the proper elevation and rejoined to the original DEM raster. The effect of trees can be excluded because of their scarcity in the studied area, and because their existence is limited just to both sides of the artificially elevated streets and areas where people live. Furthermore, the bias in the SRTM model is eliminated by two steps: (1) the mean (value) of the differences between the GCPs and the corresponding points of the SRTM is subtracted from SRTM points, and then the root mean square error (RMSE) is diminished to 0.67 m; (2) the same mean (value) of the differences is subtracted from the whole SRTM model. The finally modified DEM represents the real terrain surface with the most important details of the study area. This modified elevation model may be used in studies to model groundwater flow driven by topography.</description><subject>Agricultural research</subject><subject>Agriculture</subject><subject>Charge</subject><subject>Computer based modeling</subject><subject>Consultancy services</subject><subject>Digital Elevation Models</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Elevation</subject><subject>Embankments</subject><subject>Equator</subject><subject>Groundwater flow</subject><subject>Mounds</subject><subject>Pixels</subject><subject>Radiometry</subject><subject>Roads</subject><subject>Satellite imagery</subject><subject>Statistical methods</subject><subject>Studies</subject><subject>Topography</subject><subject>지질학</subject><issn>1226-4806</issn><issn>1598-7477</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNp1kU9P3DAQxS3UStClH4CbpR4Kh5SxvYk3R0T5J4EqIThbs85417tJnNpZKr493oZDVYnTs55_b6SZx9iJgB8CQJ8nIRWoAkRZAEgo9AE7EmW9KPRc60_5LWVVzBdQHbIvKW0ASq1AH7HtQ2i88xZHH3oeHEfe-JUfseXU0stkd6Ghlp_-vHo4477PiGtx5GMYwirisPaWYyTkf_y45pHSQHb_yzvsO2yIO8Jxl_1j9tlhm-jru87Y8_XV0-Vtcf_r5u7y4r6waiHGoqnlkmSpScjKlvPaLik7tdZg82o41wtaKsDKgSblhBWlXgrnpK1UJQlBzdj3aW4fndlabwL6v7oKZhvNxePTnZFK1CqTpxM5xPB7R2k0nU-W2hZ7CrtkhK6VVFJmmbFv_6GbsIt93iNTZT4ySKEzJSbKxpBSJGeG6DuMr0aA2RdlpqJMLsrsizL7jJwyKbP9iuI_kz8MvQHd6pQm</recordid><startdate>20160201</startdate><enddate>20160201</enddate><creator>Kanoua, Wael</creator><creator>Merkel, Broder J.</creator><general>The Geological Society of Korea</general><general>Springer Nature B.V</general><general>한국지질과학협의회</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2P</scope><scope>M7S</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>ACYCR</scope></search><sort><creationdate>20160201</creationdate><title>Modification of a digital elevation model (DEM) in a flat topographic area with respect to manmade features</title><author>Kanoua, Wael ; Merkel, Broder J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c381t-d92be257e126c549cbe92b9770c002a478eb30a6f07e3f1c157b1ff2c6362ea03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Agricultural research</topic><topic>Agriculture</topic><topic>Charge</topic><topic>Computer based modeling</topic><topic>Consultancy services</topic><topic>Digital Elevation Models</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Elevation</topic><topic>Embankments</topic><topic>Equator</topic><topic>Groundwater flow</topic><topic>Mounds</topic><topic>Pixels</topic><topic>Radiometry</topic><topic>Roads</topic><topic>Satellite imagery</topic><topic>Statistical methods</topic><topic>Studies</topic><topic>Topography</topic><topic>지질학</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kanoua, Wael</creatorcontrib><creatorcontrib>Merkel, Broder J.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>Advanced Technologies & Aerospace Database (1962 - current)</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>ProQuest advanced technologies & aerospace journals</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering collection</collection><collection>ProQuest Central Basic</collection><collection>Korean Citation Index</collection><jtitle>Geosciences journal (Seoul, Korea)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kanoua, Wael</au><au>Merkel, Broder J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Modification of a digital elevation model (DEM) in a flat topographic area with respect to manmade features</atitle><jtitle>Geosciences journal (Seoul, Korea)</jtitle><stitle>Geosci J</stitle><date>2016-02-01</date><risdate>2016</risdate><volume>20</volume><issue>1</issue><spage>101</spage><epage>115</epage><pages>101-115</pages><issn>1226-4806</issn><eissn>1598-7477</eissn><abstract>This study compares two Digital Elevation Models (DEMs) that are available free of charge: (1) the Consultative Group for International Agriculture Research Consortium for Spatial Information SRTM C-band CGIAR-CSI v4.1 (SRTM): 3 arc sec (approximately 92 m at the equator; originally 1 arc sec but only distributed with 3 arc sec) and (2) the Advanced Spaceborne Thermal Emission and Reflection Radiometer-Global Digital Elevation Model ASTER GDEM v2 (ASTER2): 1 arc sec (approximately 31 m at the equator). Additionally, the DEM was modified according to known topographic features in the study area. The first step was investigating whether there is a spatial shift between the different DEMs by using a very high resolution (VHR) satellite GeoEye image. Beside visual comparisons, statistical methods were applied to compare the elevation models. Reference data used in this study are the Ground Control Points (GCPs) collected in a previous investigation in the same study area. SRTM proved to be the better of two available free elevation models (SRTM and ASTER2). This conclusion is based on an assessment of the different investigated aspects such as morphologic details, reliability, completeness, and accuracy. The ability to modify the SRTM model with 92 m horizontal resolution from the Shuttle Radar Topography Mission is here discussed. The study area is located in Titas Upazila, Comilla district, Bangladesh and comprises manmade topographic features (e.g., road embankments and mounds that houses are built on above the monsoon flooding level), which are not or not completely represented in the DEM due to their small spatial extent. To represent these topographic features, the DEM was refined by dividing each pixel into 0.5 m pixel spacings. The elevated areas (roads and villages) were digitized using GeoEye satellite imagery and Google Earth. The pixels located in the elevated areas were given the proper elevation and rejoined to the original DEM raster. The effect of trees can be excluded because of their scarcity in the studied area, and because their existence is limited just to both sides of the artificially elevated streets and areas where people live. Furthermore, the bias in the SRTM model is eliminated by two steps: (1) the mean (value) of the differences between the GCPs and the corresponding points of the SRTM is subtracted from SRTM points, and then the root mean square error (RMSE) is diminished to 0.67 m; (2) the same mean (value) of the differences is subtracted from the whole SRTM model. The finally modified DEM represents the real terrain surface with the most important details of the study area. This modified elevation model may be used in studies to model groundwater flow driven by topography.</abstract><cop>Seoul</cop><pub>The Geological Society of Korea</pub><doi>10.1007/s12303-015-0020-7</doi><tpages>15</tpages></addata></record> |
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subjects | Agricultural research Agriculture Charge Computer based modeling Consultancy services Digital Elevation Models Earth and Environmental Science Earth Sciences Elevation Embankments Equator Groundwater flow Mounds Pixels Radiometry Roads Satellite imagery Statistical methods Studies Topography 지질학 |
title | Modification of a digital elevation model (DEM) in a flat topographic area with respect to manmade features |
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