Full text: Proceedings; XXI International Congress for Photogrammetry and Remote Sensing (Part B4-3)

WIÊÈËmÎÈÎÊËÊÊÊÈ 
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part B4. Beijing 2008 
difference between CDED level 1 and SRTM data of Mount 
Carleton is described as follows: Mean error -1.2 ± 15.6 m, 
absolute error 12.1 m, RMSE 15.6 m, Cl 51.2 m, LE 30.5 m 
with 95% of the points to present difference with the range [- 
50.0, 47.0 m]. We founded that vertical accuracy is terrain class 
dependent. Accuracy particularly suffers on terrain with slope 
values higher than 15°. High errors of CDED level 1 are not 
typical of sloping regions. Aspect of the terrain influences both 
the magnitude and the sign of errors in the difference between 
CDED level 1 and SRTM data. But statistically, limited to our 
study area, we can only mention the relative concentration of 
errors in the NE and N directions. The obtained results proved 
that the error is relatively geographic dependent in NE, N 
directions and minimized in the other directions. Like other 
DEM, CDED are slope-dependent. Mostly for SRTM model, 
their accuracy vary in function of the specific vegetation type 
(Miliaresis G.C et al. 2005). The role of vegetation was also 
assessed in our study. It is shown that in the geographic area 
studied, vegetation covers uniformly (various species) 36 x 24 
km. Differences are concentrated on broadleaf and there is not a 
correlation between the percentage of dominant species and 
large range difference. The highest RMSE of 12.7 m among 
species is for broadleaf class which is not dominant in the study 
area. Assessment of the impact of the vegetation was made 
using SRTM (CGIAR-CSI SRTM) and ICESat data. Both 
SRTM and ICESat are subject of the influence of the vegetation. 
We observed that SRTM is much closed to ICESat, but the 
RMSE of 12.7 m confirm the accuracy of ICESat data versus 
CDED level 1. The Pearson's correlation between ICESat and 
CDED level 1, the tendency of the ICESat’profiles indicated 
that data investigated in our study is reliable. 
REFERENCES 
Aguilar F. J and al.; 2005. Effects of terrain morphology, 
sampling, density, and interpolation methods on grid DEM 
accuracy. Photogrammetric Engineering & Remote Sensing 
Journal. Vol 71. N.7 p. 805 - 816 
ASPRS, 1990. American Society for Photogrammetry and 
Remote Sensing: Accuracy standards for large-scale maps. 
Photogrammetric Engineering and Remote Sensing Journal 56 
(7), pp 1068-1070 
Automated Mapping of Land Components from Digital 
Elevation Data. Earth Surface Processes and Landforms 
20:131-137 
Beaulieu Alexandre and Clavet Daniel., 2007. Accuracy 
assessment of Canadian Digital Elevation Data using ICESAT. 
Centre d’information Topographique de Sherbrooke, Québec, 
Canada. 
Braun Alexander and Georgia Fotopoulos.; 2007. Assessment 
of SRTM, ICESat and survey control monument elevations in 
Canada. Photogrammetric Engineering & Remote Sensing 
Journal. Vol 73. N.12 p. 1333 - 1345 
Burrough A. et al., 1991. Principles of Geographic Information 
Systems for Land Resources Assessment, Clarendon Press, 
Oxford. 
Carabajal C. C. et al., 2005. ICESat validation of SRTM C-band 
digital elevation models. Geophysical Research Letters 33, 
L22S01. 
Carlisle Bruce et al., 1996. The accuracy of a mountain DEM: 
Research in Snowdonia, North Wales, UK. International 
symposium on high mountain remote sensing cartography, 
Karlstad, Kiruna. 
Chrysoulakis N et al., 2006. SRTM vs ASTER elevation 
products. Comparison for two regions in Crete, Greece. 
International Journal of Remote Sensing, Vol 27, N. 10, pp 
4819-4838. 
Dymond, J. R., DeRose, R.C. & Harmsworth, G. R. (1995a). 
Fricker, H.A et al., 2005. Assessment of ICESat performance at 
the salar de Uyuni, Bolivia. Geophysical Research Letters 32, 
(21). 
George Ch. Miliaresis et al., 2005. Vertical accuracy of the 
SRTM DTED level of Crete. International Journal of Applied 
Earth Observation and Geoinformation 7, pp 49-59. 
Gorokhvich Y. et al., 2006. Accuracy assessment of the 
processed SRTM-based elevation data by using field data from 
USA and Thailand and its relation to the terrain characteristics. 
Remote Sensing of Environment 104, pp 409-415. 
Harding D.J 2005. ICESat waveform measurements of within- 
footprint topographic relief and vegetation vertical structure. 
Geophysical Research Letters, 32 L21S10. 
Hodgson Michael E. et al., 2003. An evaluation of LIDAR-and 
IFSAR-derived digital elevation models in leaf-on conditions 
with USGS Level 1 and Level 2 DEMs. Remote Sensing of 
Environment 84, pp 295-308. 
http://atlas.nrcan.gc.ca/site/english/maps/reference/provincesterr 
itoriesrelief/newbrunswick/referencemapimageview 
(Accessed 02 April 08) 
http://www.cits.mcan.gc.ca/cit/servlet/CIT?site_id=l&page_id= 
1-005-002-002 (Accessed 30 April 08) 
http://www.cits.mean.gc.ca/fich_ext/l/text/products/dnec/cdeds 
pec.pdf (Accessed 16 April 08). 
http://www. geobase. ca/geobase/en/ data/ cded/description. html ;j s 
essionid=822DA66FA 1CAF160842F139A2E346F47 (accessed 
30 April 08). 
Jarvis A., H.l Reuter, A. Nelson, E.Guevara, 2006. Hole-filled 
seamless SRTM data V3, International Centre for topographical 
Agriculture (CIAT), available from http://srtm.csi.cgiar.org. 
Lang. H. et al., 1999. ASTER digital elevation models (ATBD- 
AST-08). The Earth Observing System, Goddard Space Flight 
Center. 
Maune D.F. et al., 2001. Digital Elevation Model Technologies 
and Applications: The DEM Users Manual. American Society 
for photogrammetry and Remote Sensing, Bethesda, MD. 
Schütz. B.E et al., 2005. Overview of the ICESat Mission. 
Geographical Research Letters 32, (22) 
Sun G. et al., 2008. Forest structure from GLAS: An evaluation 
using LVIS and SRTM data. Remote Sensing of Environment 
112, pp 107-117. 
1429
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.