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G. Miliaresis, C. Paraschou (2005)
Vertical accuracy of the SRTM DTED level 1 of CreteInternational Journal of Applied Earth Observation and Geoinformation, 7
A. Hirano, R. Welch, H. Lang (2003)
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Specification for Aerophotogrammetric Office Operation
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1:25 000, 1:50 000 and 1:100 000 Topographic Maps -Specification for
P.A.M. Berry, J. Garlick, R.G. Smith (2007)
Near-global validation of the SRTM DEM using satellite radar altimetryRemote Sensing of Environment, 106
A. Racoviteanu, W. Manley, Y. Arnaud, M. Williams (2007)
Evaluating digital elevation models for glaciologic applications: An example from Nevado Coropuna, Peruvian AndesGlobal and Planetary Change, 59
Andrew Jarvis, H. Reuter, A. Nelson, E. Guevara (2008)
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Validation of digital elevation models from SRTM X-SAR for applications in hydrologic modelingIsprs Journal of Photogrammetry and Remote Sensing, 60
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Accuracy assessment of automatically derived digital elevation models from aster data in mountainous terrainInternational Journal of Remote Sensing, 26
Jiao Wen (2002)
The Origin Vertical Shift of National Height Datum 1985 with respect to the Geoidal Surface
C. Siart, O. Bubenzer, B. Eitel (2009)
Combining digital elevation data (SRTM/ASTER), high resolution satellite imagery (Quickbird) and GIS for geomorphological mapping: A multi-component case study on Mediterranean karst in Central CreteGeomorphology, 112
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ASTER Global DEM Validation Summary Report
The digital elevation model (DEM) produced by the Shuttle Radar Topographic Mission (SRTM) has provided important fundamental data for topographic analysis in many fields. The recently released global digital elevation model (GDEM) produced by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) has higher spatial resolution and wider coverage than the SRTM3 DEM, and thus may be of more value to researchers. Taking two typical study areas—the Loess Plateau and the North China Plain of China—as an example, this article assesses the accuracy of the SRTM3 DEM and ASTER GDEM by collecting ground control points from topographical maps. It is found that both the SRTM3 DEM and the ASTER GDEM are far more accurate for the North China Plain than for the Loess Plateau. For the Loess Plateau, the accuracy of the ASTER GDEM is similar to that of the SRTM3 DEM; whereas for the North China Plain, it is much worse than that of the SRTM3 DEM. Considering the negative bias of the ASTER GDEM for flat or gentle regions, we improve its accuracy by adding the difference of the mean value between the SRTM3 DEM and ASTER GDEM for the North China Plain; then, the root mean square error (RMSE) of ±7.95 m from the original ASTER GDEM is improved to ±5.26 m, which demonstrates that it is a simple but useful way to improve the accuracy of the ASTER GDEM in flat or gentle regions.
International Journal of Remote Sensing – Taylor & Francis
Published: Dec 10, 2011
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