Validation of Digital Elevation Models around Merapi Volcano, Java, Indonesia

The accuracy of 4 Digital Elevation Models (SRTM30, GTOPO30, SRTM3 and local DEM produced from aerial photogrammetric images) for the volcanoes Merapi and Merbabu in Java, Indonesia is investigated by comparison with 443 GPS ground control points. The study confirms the high accuracy of SRTM3 and SR...

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Main Authors: C. Gerstenecker, G. Läufer, D. Steineck, C. Tiede, B. Wrobel
Format: Article
Language:English
Published: Copernicus Publications 2005-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/5/863/2005/nhess-5-863-2005.pdf
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spelling doaj-cefb89b7d56b44e58f6ed3e58d120ba32020-11-24T23:57:22ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812005-01-0156863876Validation of Digital Elevation Models around Merapi Volcano, Java, IndonesiaC. GersteneckerG. LäuferD. SteineckC. TiedeB. WrobelThe accuracy of 4 Digital Elevation Models (SRTM30, GTOPO30, SRTM3 and local DEM produced from aerial photogrammetric images) for the volcanoes Merapi and Merbabu in Java, Indonesia is investigated by comparison with 443 GPS ground control points. The study confirms the high accuracy of SRTM3 and SRTM30, even if the a priori defined 90% confidence level of 16 m for the SRTM3 is not always achieved in this mountainous region. Accuracy of SRTM30, GTOPO30 and SRTM3 is mainly dependent on the altitude itself and the slopes' inclinations, whereas the photogrammetric DEM exhibits constant accuracy over a wide range of altitudes and slopes. For SRTM3 and SRTM30 a statistically significant correlation between heights and aspects of the slopes is also found. </p><p style='line-height: 20px;'> Accuracy of DEMs which are generated by interpolation on a finer grid does not change significantly. Smoothing of DEMs on a coarser grid, however, decreases accuracy. The decrease in accuracy is again dependent on altitude and slope inclination. </p><p style='line-height: 20px;'> The comparison of SRTM30 with GTOPO30 exhibits a significant improvement of SRTM30 data.http://www.nat-hazards-earth-syst-sci.net/5/863/2005/nhess-5-863-2005.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Gerstenecker
G. Läufer
D. Steineck
C. Tiede
B. Wrobel
spellingShingle C. Gerstenecker
G. Läufer
D. Steineck
C. Tiede
B. Wrobel
Validation of Digital Elevation Models around Merapi Volcano, Java, Indonesia
Natural Hazards and Earth System Sciences
author_facet C. Gerstenecker
G. Läufer
D. Steineck
C. Tiede
B. Wrobel
author_sort C. Gerstenecker
title Validation of Digital Elevation Models around Merapi Volcano, Java, Indonesia
title_short Validation of Digital Elevation Models around Merapi Volcano, Java, Indonesia
title_full Validation of Digital Elevation Models around Merapi Volcano, Java, Indonesia
title_fullStr Validation of Digital Elevation Models around Merapi Volcano, Java, Indonesia
title_full_unstemmed Validation of Digital Elevation Models around Merapi Volcano, Java, Indonesia
title_sort validation of digital elevation models around merapi volcano, java, indonesia
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2005-01-01
description The accuracy of 4 Digital Elevation Models (SRTM30, GTOPO30, SRTM3 and local DEM produced from aerial photogrammetric images) for the volcanoes Merapi and Merbabu in Java, Indonesia is investigated by comparison with 443 GPS ground control points. The study confirms the high accuracy of SRTM3 and SRTM30, even if the a priori defined 90% confidence level of 16 m for the SRTM3 is not always achieved in this mountainous region. Accuracy of SRTM30, GTOPO30 and SRTM3 is mainly dependent on the altitude itself and the slopes' inclinations, whereas the photogrammetric DEM exhibits constant accuracy over a wide range of altitudes and slopes. For SRTM3 and SRTM30 a statistically significant correlation between heights and aspects of the slopes is also found. </p><p style='line-height: 20px;'> Accuracy of DEMs which are generated by interpolation on a finer grid does not change significantly. Smoothing of DEMs on a coarser grid, however, decreases accuracy. The decrease in accuracy is again dependent on altitude and slope inclination. </p><p style='line-height: 20px;'> The comparison of SRTM30 with GTOPO30 exhibits a significant improvement of SRTM30 data.
url http://www.nat-hazards-earth-syst-sci.net/5/863/2005/nhess-5-863-2005.pdf
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