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Vertical accuracy of the SRTM DTED level 1 of Crete

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dc.contributor.author Miliaresis, GCh en
dc.contributor.author Paraschou, CVE en
dc.date.accessioned 2014-03-01T01:23:19Z
dc.date.available 2014-03-01T01:23:19Z
dc.date.issued 2005 en
dc.identifier.issn 0303-2434 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/16907
dc.subject Accuracy en
dc.subject Digital elevation models en
dc.subject Interferometric synthetic aperture radar en
dc.subject SRTM en
dc.subject Terrain analysis en
dc.subject Terrain segmentation en
dc.subject.classification Remote Sensing en
dc.subject.other accuracy assessment en
dc.subject.other digital elevation model en
dc.subject.other digital terrain model en
dc.subject.other synthetic aperture radar en
dc.subject.other Crete en
dc.subject.other Eastern Hemisphere en
dc.subject.other Eurasia en
dc.subject.other Europe en
dc.subject.other Greece en
dc.subject.other Southern Europe en
dc.subject.other World en
dc.title Vertical accuracy of the SRTM DTED level 1 of Crete en
heal.type journalArticle en
heal.identifier.primary 10.1016/j.jag.2004.12.001 en
heal.identifier.secondary http://dx.doi.org/10.1016/j.jag.2004.12.001 en
heal.language English en
heal.publicationDate 2005 en
heal.abstract A reference digital elevation model (DEM), produced from contour lines digitization, from topographic maps at scale 1:250.000 is used in order to assess the vertical accuracy of the SRTM DTED level 1 in Crete Island in Southern Greece. The error image interpretation revealed three types of systematic errors: (a) stripping, (b) large voids and (c) those errors resulted from the mis-registration of the Shuttle Radar Topography Mission (SRTM) imagery to the local datum. Terrain was segmented to plane regions and sloping regions. Sloping regions were segmented to aspect regions (aspect being standardized to the eight geographic directions defined in a raster/grid image). Error statistics was computed for the study area as well as the individual terrain classes. Vertical accuracy was found to be terrain class dependent. Sloping regions present greater mean error than the plane ones. Statistical tests verified that the difference in mean error between aspect regions that slope in opposite geographic directions is statistically significant. The greater mean error is observed for SW, W and NW aspect regions. The additional finishing steps applied to the SRTM dataset were not sufficient enough for the systematic errors and the terrain class dependency of the error to be corrected. The observed root-mean-square error (RMSE) for the SRTM DTED-1 of Crete do not fulfil the 16 m RMSE specification for the SRTM mission while the USA national map accuracy standards for the scale 1:250.000 are satisfied. (c) 2005 Elsevier B.V. All rights reserved. en
heal.publisher ELSEVIER SCIENCE BV en
heal.journalName International Journal of Applied Earth Observation and Geoinformation en
dc.identifier.doi 10.1016/j.jag.2004.12.001 en
dc.identifier.isi ISI:000231697600004 en
dc.identifier.volume 7 en
dc.identifier.issue 1 en
dc.identifier.spage 49 en
dc.identifier.epage 59 en


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